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		<title>In Most Zones Of Continent-continent Collision - Versionsgeschichte</title>
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		<title>MichaelaSwisher am 27. Oktober 2025 um 14:06 Uhr</title>
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				<updated>2025-10-27T14:06:18Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;← Nächstältere Version&lt;/td&gt;
			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 27. Oktober 2025, 14:06 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;type &lt;/del&gt;of tectonics that's dominated by lateral (horizontal) movements &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics forms the boundary between two tectonic plates, this is known as a remodel or conservative plate boundary. Areas of strike-slip tectonics are characterised by &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;explicit &lt;/del&gt;deformation &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;styles together with&lt;/del&gt;: &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://152.136.126.252:3000/camillejowett/camille2004/wiki/Hair-Cutting-Scissors-for-The-Professional-Hair-Stylist Wood Ranger official] &lt;/del&gt;stepovers, Riedel [https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;asteroidsathome&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;net&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;boinc/view_profile.php?userid=868657 &lt;/del&gt;Wood Ranger Power Shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;USA&lt;/del&gt;], flower &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructions &lt;/del&gt;and strike-slip duplexes. Where the displacement &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;along &lt;/del&gt;a zone of strike-slip deviates from parallelism with the zone itself, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;style &lt;/del&gt;becomes both transpressional or transtensional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;depending &lt;/del&gt;on the sense of deviation. Strike-slip tectonics is characteristic of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;several &lt;/del&gt;geological environments, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;together with &lt;/del&gt;oceanic and continental &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/del&gt;faults, zones of oblique collision and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://mqbinfo.com/w/User:Modesta70U Wood Ranger official] &lt;/del&gt;the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;typically kind &lt;/del&gt;as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a number of &lt;/del&gt;separate fault segments &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;that are &lt;/del&gt;offset from one another. The areas between the ends of adjoining segments are referred to as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Within the case of a dextral fault zone, a proper-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/del&gt;an extensional stepover as movement on the 2 segments leads to extensional deformation &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/del&gt;the zone of offset, while a left-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;a compressional stepover. For &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lively &lt;/del&gt;strike-slip techniques, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://nccproduction.com/wiki/in_case_you_suspect_a_f_eon_p_oblem Wood Ranger official] &lt;/del&gt;earthquake ruptures may jump from one phase to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a different across &lt;/del&gt;the intervening stepover, if the offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;just &lt;/del&gt;not too &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;nice&lt;/del&gt;. Numerical modelling has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;steered &lt;/del&gt;that jumps of no less than &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;8 &lt;/del&gt;km, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://torrdan.net:80/index.php?title=Not_What_You_re_Searching_For Wood Ranger official] &lt;/del&gt;or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;probably extra &lt;/del&gt;are possible. This is backed up by &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;evidence &lt;/del&gt;that the rupture of the 2001 Kunlun earthquake jumped &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;more &lt;/del&gt;than 10 km &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/del&gt;an extensional stepover. The presence of stepovers &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in the course of &lt;/del&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;earthquake rupture. Within the early &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;phases &lt;/del&gt;of strike-slip fault formation, displacement &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;basement rocks produces characteristic fault structures within the overlying &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cowl&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;This may even be the case &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;where &lt;/del&gt;an energetic strike-slip zone lies within an area of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;persevering with &lt;/del&gt;sedimentation. At low levels of pressure, the overall simple shear causes a set of small faults to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;form&lt;/del&gt;. The dominant set, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;often called &lt;/del&gt;R &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://wiki.fuzokudb.com/fdb/Scissors_Aren%E2%80%99t_Shears:_Why_Tool_Quality_And_Maintenance_Matter_More_Than_You_Think Wood Ranger Power Shears review]&lt;/del&gt;,&amp;#160; [https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;koreanaggies&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;net&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;board_Lmao72&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;1959139 &lt;/del&gt;Wood Ranger &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;official&lt;/del&gt;] &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;forms &lt;/del&gt;at about 15° to the underlying fault with the identical shear sense. The R [https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;www&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;yewiki&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;org&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Should_You_Choose_Double-Cut_Shears_Or_Single-Cut_Shears power &lt;/del&gt;shears] are then linked by a second set, the R' &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://freekoreatravel.com/index.php/The_Eight_Best_Tree_Loppers_Of_2025 Wood Ranger Power Shears for sale]&lt;/del&gt;, that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/del&gt;at about 75° to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;primary &lt;/del&gt;fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;trace&lt;/del&gt;. These two fault orientations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/del&gt;be understood as conjugate fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;units &lt;/del&gt;at 30° to the quick axis of the instantaneous &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/del&gt;ellipse related to the simple shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;strain area attributable to &lt;/del&gt;the displacements &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;utilized &lt;/del&gt;at the bottom of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/del&gt;sequence. With further displacement, the Riedel fault segments will &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;are inclined &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;turn &lt;/del&gt;into &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fully &lt;/del&gt;linked &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;till &lt;/del&gt;a throughgoing fault is formed. The linkage usually occurs with the event of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a further &lt;/del&gt;set of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://azbongda.com/index.php/Top_Q0_Best_Japanese_Shears_In_2025 Wood Ranger Power Shears shop] &lt;/del&gt;generally known as 'P shears', which are roughly symmetrical to the R shears relative to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;general &lt;/del&gt;shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;route&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The somewhat oblique segments will link downwards into the fault at the bottom of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/del&gt;sequence with a helicoidal geometry. Intimately, many strike-slip faults at &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;floor consist of &lt;/del&gt;en echelon or braided segments, which in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;many instances have &lt;/del&gt;been &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;most likely &lt;/del&gt;inherited from &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;beforehand &lt;/del&gt;formed Riedel shears. In cross-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;part&lt;/del&gt;, the displacements are dominantly reverse or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;regular &lt;/del&gt;in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sort &lt;/del&gt;depending on whether the overall fault geometry is transpressional (i.e. with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;element &lt;/del&gt;of shortening) or transtensional (with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;component &lt;/del&gt;of extension). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;As &lt;/del&gt;the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;tend &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;affix &lt;/del&gt;downwards onto a single strand in basement, the geometry has led to these being termed flower construction. Fault zones with dominantly reverse faulting are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;positive flowers, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;while these &lt;/del&gt;with dominantly &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;regular &lt;/del&gt;offsets are often called &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;unfavourable &lt;/del&gt;flowers. The identification of such buildings, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;particularly the place &lt;/del&gt;optimistic and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;detrimental &lt;/del&gt;flowers are developed on &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;totally &lt;/del&gt;different segments of the same fault, are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;thought to be &lt;/del&gt;reliable indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes happen at the stepover &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;areas &lt;/del&gt;of faults, forming lens-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;formed &lt;/del&gt;near parallel arrays of horses. These &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;occur &lt;/del&gt;between two or extra large bounding faults which often have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;large &lt;/del&gt;displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;solely &lt;/del&gt;horizontal &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/del&gt;, thus there &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;isn't any &lt;/del&gt;change in topography &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;as a result &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/del&gt;of the fault. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;actuality&lt;/del&gt;, as strike-slip faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;turn out &lt;/del&gt;to be giant and developed, their &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;behavior&amp;#160; [https://seven.mixh.jp/answer/question/dokan-grass-shears-hand-made-small-wood-handle-offset-shears-100mm Wood Ranger official] &lt;/del&gt;adjustments and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;becomes &lt;/del&gt;more &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;complicated&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;An extended &lt;/del&gt;strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that comply with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;primary &lt;/del&gt;fault direction. These sub-parallel stretches are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;remoted &lt;/del&gt;by offsets at first, but over long &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;periods &lt;/del&gt;of time, they can &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;turn out &lt;/del&gt;to be related by stepovers to accommodate the strike-slip displacement. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lengthy &lt;/del&gt;stretches of strike-slip, the fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;aircraft &lt;/del&gt;can start to curve, giving rise to constructions &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;much like &lt;/del&gt;step overs. Right lateral motion of a strike-slip fault at a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;right &lt;/del&gt;stepover (or overstep) offers rise to extensional bends characterised by zones of subsidence, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;local &lt;/del&gt;normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;kind &lt;/ins&gt;of tectonics that's dominated by lateral (horizontal) movements &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics forms the boundary between two tectonic plates, this is known as a remodel or conservative plate boundary. Areas of strike-slip tectonics are characterised by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;specific &lt;/ins&gt;deformation &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;kinds including&lt;/ins&gt;: stepovers, Riedel [https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;urllink&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;me&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;jacelynfelder9 &lt;/ins&gt;Wood Ranger Power Shears &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shop&lt;/ins&gt;], flower &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;buildings &lt;/ins&gt;and strike-slip duplexes. Where the displacement &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;alongside &lt;/ins&gt;a zone of strike-slip deviates from parallelism with the zone itself, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;type &lt;/ins&gt;becomes both transpressional or transtensional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;relying &lt;/ins&gt;on the sense of deviation. Strike-slip tectonics is characteristic of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a number of &lt;/ins&gt;geological environments, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;including &lt;/ins&gt;oceanic and continental &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;remodel &lt;/ins&gt;faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sometimes type &lt;/ins&gt;as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;several &lt;/ins&gt;separate fault segments &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;which can be &lt;/ins&gt;offset from one another. The areas between the ends of adjoining segments are referred to as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Within the case of a dextral fault zone, a proper-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/ins&gt;an extensional stepover as movement on the 2 segments leads to extensional deformation &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the zone of offset, while a left-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/ins&gt;a compressional stepover. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;active &lt;/ins&gt;strike-slip techniques, earthquake ruptures may jump from one phase to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;another throughout &lt;/ins&gt;the intervening stepover, if the offset is not too &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;great&lt;/ins&gt;. Numerical modelling has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;recommended &lt;/ins&gt;that jumps of no less than &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;eight &lt;/ins&gt;km, or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;presumably more &lt;/ins&gt;are possible. This is backed up by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;proof &lt;/ins&gt;that the rupture of the 2001 Kunlun earthquake jumped &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;greater &lt;/ins&gt;than 10 km &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;an extensional stepover. The presence of stepovers &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;during &lt;/ins&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;during &lt;/ins&gt;earthquake rupture. Within the early &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;levels &lt;/ins&gt;of strike-slip fault formation, displacement &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;inside &lt;/ins&gt;basement rocks produces characteristic fault structures within the overlying &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cover&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;This may even be the case &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the place &lt;/ins&gt;an energetic strike-slip zone lies within an area of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;continuing &lt;/ins&gt;sedimentation. At low levels of pressure, the overall simple shear causes a set of small faults to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;type&lt;/ins&gt;. The dominant set, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;generally known as &lt;/ins&gt;R &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/ins&gt;,&amp;#160; [https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;morphomics&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;science&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;The_KitchenAid_Shears_Hit_All-time_Low_Price_Before_October_Prime_Day &lt;/ins&gt;Wood Ranger &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;brand shears&lt;/ins&gt;] &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;varieties &lt;/ins&gt;at about 15° to the underlying fault with the identical shear sense. The R [https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;gitea&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;mxthome&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;ru&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;theresaburton Wood Ranger brand &lt;/ins&gt;shears] are then linked by a second set, the R' &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/ins&gt;, that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;varieties &lt;/ins&gt;at about 75° to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;principle &lt;/ins&gt;fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;hint&lt;/ins&gt;. These two fault orientations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;will &lt;/ins&gt;be understood as conjugate fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sets &lt;/ins&gt;at 30° to the quick axis of the instantaneous &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;strain &lt;/ins&gt;ellipse related to the simple shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressure subject caused by &lt;/ins&gt;the displacements &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;applied &lt;/ins&gt;at the bottom of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/ins&gt;sequence. With further displacement, the Riedel fault segments will &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;tend &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;change &lt;/ins&gt;into &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;absolutely &lt;/ins&gt;linked &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;until &lt;/ins&gt;a throughgoing fault is formed. The linkage usually occurs with the event of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;an extra &lt;/ins&gt;set of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shears &lt;/ins&gt;generally known as 'P shears', which are roughly symmetrical to the R shears relative to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;overall &lt;/ins&gt;shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;direction&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The somewhat oblique segments will link downwards into the fault at the bottom of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/ins&gt;sequence with a helicoidal geometry. Intimately, many strike-slip faults at &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;surface include &lt;/ins&gt;en echelon or braided segments, which in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;lots of cases had &lt;/ins&gt;been &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;probably &lt;/ins&gt;inherited from &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/ins&gt;formed Riedel shears. In cross-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;section&lt;/ins&gt;, the displacements are dominantly reverse or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;normal &lt;/ins&gt;in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;type &lt;/ins&gt;depending on whether &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;or not &lt;/ins&gt;the overall fault geometry is transpressional (i.e. with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;component &lt;/ins&gt;of shortening) or transtensional (with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;part &lt;/ins&gt;of extension). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Because &lt;/ins&gt;the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;have a tendency &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;hitch &lt;/ins&gt;downwards onto a single strand in basement, the geometry has led to these being termed flower construction. Fault zones with dominantly reverse faulting are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;often called &lt;/ins&gt;positive flowers, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;whereas those &lt;/ins&gt;with dominantly &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;normal &lt;/ins&gt;offsets are often called &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;negative &lt;/ins&gt;flowers. The identification of such buildings, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;notably where &lt;/ins&gt;optimistic and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;unfavorable &lt;/ins&gt;flowers are developed on different segments of the same fault, are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;considered &lt;/ins&gt;reliable indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes happen at the stepover &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;regions &lt;/ins&gt;of faults, forming lens-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shaped &lt;/ins&gt;near parallel arrays of horses. These &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;happen &lt;/ins&gt;between two or extra large bounding faults which often have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;giant &lt;/ins&gt;displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;only &lt;/ins&gt;horizontal &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/ins&gt;, thus there &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is no such thing as a &lt;/ins&gt;change in topography &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;because &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/ins&gt;of the fault. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;reality&lt;/ins&gt;, as strike-slip faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;grow &lt;/ins&gt;to be giant and developed, their &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;habits &lt;/ins&gt;adjustments and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;turns into &lt;/ins&gt;more &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;advanced&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;A long &lt;/ins&gt;strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that comply with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;main &lt;/ins&gt;fault direction. These sub-parallel stretches are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;isolated &lt;/ins&gt;by offsets at first, but over long &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;intervals &lt;/ins&gt;of time, they can &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;grow &lt;/ins&gt;to be related by stepovers to accommodate the strike-slip displacement. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;long &lt;/ins&gt;stretches of strike-slip, the fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;plane &lt;/ins&gt;can start to curve, giving rise to constructions &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;similar to &lt;/ins&gt;step overs. Right lateral motion of a strike-slip fault at a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;proper &lt;/ins&gt;stepover (or overstep) offers rise to extensional bends characterised by zones of subsidence, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;native &lt;/ins&gt;normal faults, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://safeareamain.com/bbs/board.php?bo_table=free&amp;amp;wr_id=77774 Wood Ranger Power Shears price] [https://quickbio.click/meridithcroppe Wood Ranger Power Shears coupon] [https://git.vereint-digital.de/eugeniawiles3 cordless power shears] [https://et6.ir/kristiecavines Wood Ranger Power Shears features] website &lt;/ins&gt;and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>MichaelaSwisher</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=In_Most_Zones_Of_Continent-continent_Collision&amp;diff=119916&amp;oldid=prev</id>
		<title>XYSEmilia245 am 5. September 2025 um 05:46 Uhr</title>
		<link rel="alternate" type="text/html" href="http://www.vokipedia.de/index.php?title=In_Most_Zones_Of_Continent-continent_Collision&amp;diff=119916&amp;oldid=prev"/>
				<updated>2025-09-05T05:46:07Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 5. September 2025, 05:46 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kind &lt;/del&gt;of tectonics that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/del&gt;dominated by lateral (horizontal) movements &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/del&gt;the boundary between two tectonic plates, this is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/del&gt;a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/del&gt;or conservative plate boundary. Areas of strike-slip tectonics are characterised by &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;particular &lt;/del&gt;deformation &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/del&gt;together with: stepovers, Riedel [https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wiki.dulovic&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;tech&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;index&lt;/del&gt;.php&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;/User:BrandieMrt &lt;/del&gt;Wood Ranger Power Shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;website&lt;/del&gt;], flower &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;buildings &lt;/del&gt;and strike-slip duplexes. Where the displacement &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;alongside &lt;/del&gt;a zone of strike-slip deviates from parallelism with the zone itself, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fashion turns into &lt;/del&gt;both transpressional or transtensional &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;relying &lt;/del&gt;on the sense of deviation. Strike-slip tectonics is characteristic of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;a number of &lt;/del&gt;geological environments, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://www.vokipedia.de/index.php?title=Forms_Of_Pruning_Shears Wood Ranger Power Shears website] &lt;/del&gt;together with oceanic and continental &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rework &lt;/del&gt;faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sometimes form &lt;/del&gt;as a number of separate fault segments &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which might be &lt;/del&gt;offset from one another. The areas between the ends of adjoining segments are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;generally known &lt;/del&gt;as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;In &lt;/del&gt;the case of a dextral fault zone, a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;right&lt;/del&gt;-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;an extensional stepover as movement on the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;two &lt;/del&gt;segments leads to extensional deformation in the zone of offset, while a left-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/del&gt;a compressional stepover. For lively strike-slip techniques, earthquake ruptures may &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;bounce &lt;/del&gt;from one &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;segment &lt;/del&gt;to a different across the intervening stepover,&amp;#160; [&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;laduni.id/Quantifying_The_Impact_Of_Detection_Bias_From_Blended_Galaxies_On_Cosmic_Shear_Surveys Wood Ranger Power Shears coupon] [https&lt;/del&gt;:&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;//www.yewiki.org/Quality_Used_Machinery Wood Ranger Power Shears price] [http://classicalmusicmp3freedownload.com/ja&lt;/del&gt;/index.php?title=&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Best_Hairdressing_Scissors_2025:_Classic_Scissors_And_Thinning_Shears_For_A_Salon-High_Quality_Cut_At_Home buy &lt;/del&gt;Wood Ranger &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Power Shears&lt;/del&gt;] &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://www.koklek.go.th/question/welcome-to-recycling-equipment-corporation/ Wood Ranger Power Shears order now] order now if the offset isn't too great. Numerical modelling has instructed that jumps of a minimum of eight km, &lt;/del&gt;or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;possibly more &lt;/del&gt;are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;feasible&lt;/del&gt;. This is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped more than 10 km across an extensional stepover. The presence of stepovers &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/del&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) throughout earthquake rupture. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;In &lt;/del&gt;the early &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;levels &lt;/del&gt;of strike-slip fault formation, displacement within basement rocks produces characteristic fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructions inside &lt;/del&gt;the overlying &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cover&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;This &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;will also &lt;/del&gt;be the case &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;the place &lt;/del&gt;an &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;active &lt;/del&gt;strike-slip zone lies &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;inside &lt;/del&gt;an &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;space &lt;/del&gt;of persevering with sedimentation. At low levels of pressure, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;general &lt;/del&gt;simple shear causes a set of small faults to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;type&lt;/del&gt;. The dominant set, often &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;R &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/del&gt;at about 15° to the underlying fault with the identical shear sense. The R shears are then linked by a second set, the R' &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/del&gt;, that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kinds &lt;/del&gt;at about 75° to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;principle &lt;/del&gt;fault trace. These two fault orientations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;can &lt;/del&gt;be understood as conjugate fault units at 30° to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;brief &lt;/del&gt;axis of the instantaneous pressure ellipse related to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;straightforward &lt;/del&gt;shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure subject &lt;/del&gt;attributable to the displacements utilized at the bottom of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/del&gt;sequence. With &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;additional &lt;/del&gt;displacement, the Riedel fault segments will are inclined to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;develop &lt;/del&gt;into &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;absolutely &lt;/del&gt;linked till a throughgoing fault is formed. The linkage &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;typically happens &lt;/del&gt;with the event of a further set of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shears generally known as 'P &lt;/del&gt;[&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;viss&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;net&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cn:3000&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;rhysellwood037 &lt;/del&gt;Wood Ranger Power Shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sale&lt;/del&gt;]', &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;that &lt;/del&gt;are roughly symmetrical to the R shears relative to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;overall &lt;/del&gt;shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;path&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The somewhat oblique segments will &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;hyperlink &lt;/del&gt;downwards into the fault at the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;base &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/del&gt;sequence with a helicoidal geometry. Intimately, many strike-slip faults at &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;surface encompass &lt;/del&gt;en echelon or braided segments, which in many instances &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;were &lt;/del&gt;most likely inherited from &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/del&gt;formed Riedel shears. In cross-part, the displacements are dominantly reverse or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;normal &lt;/del&gt;in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kind &lt;/del&gt;depending on whether &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;or not &lt;/del&gt;the overall fault geometry is transpressional (i.e. with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;component &lt;/del&gt;of shortening) or transtensional (with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;part &lt;/del&gt;of extension). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Because &lt;/del&gt;the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;have a tendency &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;hitch &lt;/del&gt;downwards onto a single strand in basement, the geometry has led to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;those &lt;/del&gt;being termed flower construction. Fault zones with dominantly reverse faulting are known as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;optimistic &lt;/del&gt;flowers, while these with dominantly &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;normal &lt;/del&gt;offsets are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;generally known as damaging &lt;/del&gt;flowers. The identification of such buildings, particularly &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;where &lt;/del&gt;optimistic and detrimental flowers are developed on totally different segments of the same fault, are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;regarded as &lt;/del&gt;reliable indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;occur &lt;/del&gt;at the stepover areas of faults, forming lens-formed &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;close to &lt;/del&gt;parallel arrays of horses. These occur between two or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;more &lt;/del&gt;large bounding faults which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;usually &lt;/del&gt;have large displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has solely horizontal movement, thus there &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;is no &lt;/del&gt;change in topography as a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;consequence &lt;/del&gt;of movement of the fault. In actuality, as strike-slip faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;become &lt;/del&gt;giant and developed, their &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;habits modifications &lt;/del&gt;and becomes &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;extra &lt;/del&gt;complicated. An extended strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that comply with the primary fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;path&lt;/del&gt;. These sub-parallel stretches are remoted by offsets at first, but over long &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;intervals &lt;/del&gt;of time, they&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;'ll &lt;/del&gt;turn &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;into &lt;/del&gt;related by stepovers to accommodate the strike-slip displacement. In lengthy stretches of strike-slip, the fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;plane &lt;/del&gt;can start to curve, giving rise to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;buildings similar to &lt;/del&gt;step overs. Right lateral motion of a strike-slip fault at a right stepover (or overstep) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;gives &lt;/del&gt;rise to extensional bends characterised by zones of subsidence, local normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;type &lt;/ins&gt;of tectonics that&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/ins&gt;dominated by lateral (horizontal) movements &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;forms &lt;/ins&gt;the boundary between two tectonic plates, this is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/ins&gt;a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;remodel &lt;/ins&gt;or conservative plate boundary. Areas of strike-slip tectonics are characterised by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;explicit &lt;/ins&gt;deformation &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;styles &lt;/ins&gt;together with: &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://152.136.126.252:3000/camillejowett/camille2004/wiki/Hair-Cutting-Scissors-for-The-Professional-Hair-Stylist Wood Ranger official] &lt;/ins&gt;stepovers, Riedel [https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;asteroidsathome&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;net&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;boinc/view_profile&lt;/ins&gt;.php&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;?userid=868657 &lt;/ins&gt;Wood Ranger Power Shears &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;USA&lt;/ins&gt;], flower &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constructions &lt;/ins&gt;and strike-slip duplexes. Where the displacement &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;along &lt;/ins&gt;a zone of strike-slip deviates from parallelism with the zone itself, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;style becomes &lt;/ins&gt;both transpressional or transtensional &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;depending &lt;/ins&gt;on the sense of deviation. Strike-slip tectonics is characteristic of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;several &lt;/ins&gt;geological environments, together with oceanic and continental &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/ins&gt;faults, zones of oblique collision and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://mqbinfo.com/w/User:Modesta70U Wood Ranger official] &lt;/ins&gt;the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;typically kind &lt;/ins&gt;as a number of separate fault segments &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;that are &lt;/ins&gt;offset from one another. The areas between the ends of adjoining segments are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;referred to &lt;/ins&gt;as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Within &lt;/ins&gt;the case of a dextral fault zone, a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;proper&lt;/ins&gt;-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/ins&gt;an extensional stepover as movement on the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;2 &lt;/ins&gt;segments leads to extensional deformation in the zone of offset, while a left-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/ins&gt;a compressional stepover. For lively strike-slip techniques, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://nccproduction.com/wiki/in_case_you_suspect_a_f_eon_p_oblem Wood Ranger official] &lt;/ins&gt;earthquake ruptures may &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;jump &lt;/ins&gt;from one &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;phase &lt;/ins&gt;to a different across the intervening stepover&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;, if the offset is just not too nice. Numerical modelling has steered that jumps of no less than 8 km&lt;/ins&gt;,&amp;#160; [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;torrdan&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;net&lt;/ins&gt;:&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;80&lt;/ins&gt;/index.php?title=&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Not_What_You_re_Searching_For &lt;/ins&gt;Wood Ranger &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;official&lt;/ins&gt;] or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;probably extra &lt;/ins&gt;are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;possible&lt;/ins&gt;. This is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped more than 10 km across an extensional stepover. The presence of stepovers &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in the course of &lt;/ins&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) throughout earthquake rupture. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Within &lt;/ins&gt;the early &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;phases &lt;/ins&gt;of strike-slip fault formation, displacement within basement rocks produces characteristic fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;structures within &lt;/ins&gt;the overlying &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cowl&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;This &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;may even &lt;/ins&gt;be the case &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;where &lt;/ins&gt;an &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;energetic &lt;/ins&gt;strike-slip zone lies &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;an &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/ins&gt;of persevering with sedimentation. At low levels of pressure, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;overall &lt;/ins&gt;simple shear causes a set of small faults to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;form&lt;/ins&gt;. The dominant set, often &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/ins&gt;R &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://wiki.fuzokudb.com/fdb/Scissors_Aren%E2%80%99t_Shears:_Why_Tool_Quality_And_Maintenance_Matter_More_Than_You_Think Wood Ranger Power Shears review]&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://koreanaggies.net/board_Lmao72/1959139 Wood Ranger official] forms &lt;/ins&gt;at about 15° to the underlying fault with the identical shear sense. The R &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://www.yewiki.org/Should_You_Choose_Double-Cut_Shears_Or_Single-Cut_Shears power &lt;/ins&gt;shears&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;] &lt;/ins&gt;are then linked by a second set, the R' &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://freekoreatravel.com/index.php/The_Eight_Best_Tree_Loppers_Of_2025 Wood Ranger Power Shears for sale]&lt;/ins&gt;, that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/ins&gt;at about 75° to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;primary &lt;/ins&gt;fault trace. These two fault orientations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/ins&gt;be understood as conjugate fault units at 30° to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;quick &lt;/ins&gt;axis of the instantaneous pressure ellipse related to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;simple &lt;/ins&gt;shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;strain area &lt;/ins&gt;attributable to the displacements utilized at the bottom of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/ins&gt;sequence. With &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;further &lt;/ins&gt;displacement, the Riedel fault segments will are inclined to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;turn &lt;/ins&gt;into &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;fully &lt;/ins&gt;linked till a throughgoing fault is formed. The linkage &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;usually occurs &lt;/ins&gt;with the event of a further set of [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;azbongda&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;com/index&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;php&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Top_Q0_Best_Japanese_Shears_In_2025 &lt;/ins&gt;Wood Ranger Power Shears &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shop&lt;/ins&gt;] &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;generally known as 'P shears&lt;/ins&gt;', &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;which &lt;/ins&gt;are roughly symmetrical to the R shears relative to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;general &lt;/ins&gt;shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;route&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The somewhat oblique segments will &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;link &lt;/ins&gt;downwards into the fault at the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;bottom &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/ins&gt;sequence with a helicoidal geometry. Intimately, many strike-slip faults at &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;floor consist of &lt;/ins&gt;en echelon or braided segments, which in many instances &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;have been &lt;/ins&gt;most likely inherited from &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;beforehand &lt;/ins&gt;formed Riedel shears. In cross-part, the displacements are dominantly reverse or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;regular &lt;/ins&gt;in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sort &lt;/ins&gt;depending on whether the overall fault geometry is transpressional (i.e. with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;element &lt;/ins&gt;of shortening) or transtensional (with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;component &lt;/ins&gt;of extension). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;As &lt;/ins&gt;the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;tend &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;affix &lt;/ins&gt;downwards onto a single strand in basement, the geometry has led to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;these &lt;/ins&gt;being termed flower construction. Fault zones with dominantly reverse faulting are known as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;positive &lt;/ins&gt;flowers, while these with dominantly &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;regular &lt;/ins&gt;offsets are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;often called unfavourable &lt;/ins&gt;flowers. The identification of such buildings, particularly &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the place &lt;/ins&gt;optimistic and detrimental flowers are developed on totally different segments of the same fault, are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;thought to be &lt;/ins&gt;reliable indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;happen &lt;/ins&gt;at the stepover areas of faults, forming lens-formed &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;near &lt;/ins&gt;parallel arrays of horses. These occur between two or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;extra &lt;/ins&gt;large bounding faults which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;often &lt;/ins&gt;have large displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has solely horizontal movement, thus there &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;isn't any &lt;/ins&gt;change in topography as a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;result &lt;/ins&gt;of movement of the fault. In actuality, as strike-slip faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;turn out to be &lt;/ins&gt;giant and developed, their &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;behavior&amp;#160; [https://seven.mixh.jp/answer/question/dokan-grass-shears-hand-made-small-wood-handle-offset-shears-100mm Wood Ranger official] adjustments &lt;/ins&gt;and becomes &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;more &lt;/ins&gt;complicated. An extended strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that comply with the primary fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;direction&lt;/ins&gt;. These sub-parallel stretches are remoted by offsets at first, but over long &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;periods &lt;/ins&gt;of time, they &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;can &lt;/ins&gt;turn &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;out to be &lt;/ins&gt;related by stepovers to accommodate the strike-slip displacement. In lengthy stretches of strike-slip, the fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;aircraft &lt;/ins&gt;can start to curve, giving rise to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constructions much like &lt;/ins&gt;step overs. Right lateral motion of a strike-slip fault at a right stepover (or overstep) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;offers &lt;/ins&gt;rise to extensional bends characterised by zones of subsidence, local normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>XYSEmilia245</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=In_Most_Zones_Of_Continent-continent_Collision&amp;diff=118741&amp;oldid=prev</id>
		<title>CelsaWheeler08 am 3. September 2025 um 22:24 Uhr</title>
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				<updated>2025-09-03T22:24:31Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class='diff diff-contentalign-left'&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 3. September 2025, 22:24 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sort &lt;/del&gt;of tectonics that is dominated by lateral (horizontal) movements &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;inside &lt;/del&gt;the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;forms &lt;/del&gt;the boundary between two tectonic plates, this is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;remodel &lt;/del&gt;or conservative plate boundary. Areas of strike-slip tectonics are characterised by particular deformation &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kinds &lt;/del&gt;together with: stepovers, Riedel &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/del&gt;, flower buildings and strike-slip duplexes. Where the displacement alongside a zone of strike-slip deviates from parallelism with the zone itself, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;model &lt;/del&gt;turns into both transpressional or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://wiki.die-karte-bitte.de/index.php/Professional_Garden_Tools-Premium_Bypass_Pruners-Shears durable garden trimmer] &lt;/del&gt;transtensional relying on the sense of deviation. Strike-slip tectonics is characteristic of a number of geological environments, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;including &lt;/del&gt;oceanic and continental &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/del&gt;faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;usually type &lt;/del&gt;as a number of separate fault segments which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/del&gt;offset from one another. The areas between the ends of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;adjacent &lt;/del&gt;segments are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;referred to &lt;/del&gt;as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;In the case of a dextral fault zone, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://systemcheck-wiki.de/index.php?title=Easy_Methods_To_Make_Shears_In_Minecraft durable garden trimmer] &lt;/del&gt;a right-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/del&gt;an extensional stepover as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/del&gt;on the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;2 &lt;/del&gt;segments leads to extensional deformation in the zone of offset, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;whereas &lt;/del&gt;a left-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;a compressional stepover. For &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;energetic &lt;/del&gt;strike-slip techniques, earthquake ruptures &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;could &lt;/del&gt;bounce from one &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;phase &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;another &lt;/del&gt;across the intervening stepover, if the offset &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;just &lt;/del&gt;isn't too great. Numerical modelling has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;recommended &lt;/del&gt;that jumps of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;not less than &lt;/del&gt;eight km, or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;presumably extra &lt;/del&gt;are feasible. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;That &lt;/del&gt;is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;greater &lt;/del&gt;than 10 km &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;an extensional stepover. The presence of stepovers &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) throughout earthquake rupture. In the early levels of strike-slip fault formation, displacement within basement rocks produces characteristic fault constructions inside the overlying cover.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;It &lt;/del&gt;will &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;even &lt;/del&gt;be the case the place an &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lively &lt;/del&gt;strike-slip zone lies inside an &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/del&gt;of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;continuing &lt;/del&gt;sedimentation. At low levels of pressure, the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;overall easy &lt;/del&gt;shear causes a set of small faults to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;form&lt;/del&gt;. The dominant set, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;generally &lt;/del&gt;known as R &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[http://sinzero.xyz:3000/martyits143965 buy Wood Ranger Power Shears]&lt;/del&gt;, types at about 15° to the underlying fault with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;same &lt;/del&gt;shear sense. The R shears are then linked by a second set, the R' shears, that kinds at about 75° to the principle fault trace. These two fault orientations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;will &lt;/del&gt;be understood as conjugate fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sets &lt;/del&gt;at 30° to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;quick &lt;/del&gt;axis of the instantaneous pressure ellipse related to the straightforward shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;strain &lt;/del&gt;subject &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;caused by &lt;/del&gt;the displacements &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;applied &lt;/del&gt;at the bottom of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/del&gt;sequence. With additional displacement, the Riedel fault segments will &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;tend &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;change &lt;/del&gt;into &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;fully &lt;/del&gt;linked &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;until &lt;/del&gt;a throughgoing fault is formed. The linkage typically happens with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;development &lt;/del&gt;of a further set of shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;often called &lt;/del&gt;'P &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/del&gt;', that are roughly symmetrical to the R shears relative to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;general &lt;/del&gt;shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;course&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;considerably &lt;/del&gt;oblique segments will hyperlink downwards into the fault at the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;bottom &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/del&gt;sequence with a helicoidal geometry. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;In detail&lt;/del&gt;, many strike-slip faults at surface &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;include &lt;/del&gt;en echelon or braided segments, which in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lots of &lt;/del&gt;instances were &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;in all probability &lt;/del&gt;inherited from &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;beforehand &lt;/del&gt;formed Riedel shears. In cross-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;section&lt;/del&gt;, the displacements are dominantly reverse or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;regular &lt;/del&gt;in kind depending on whether or not the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;general &lt;/del&gt;fault geometry is transpressional (i.e. with a small component of shortening) or transtensional (with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;element &lt;/del&gt;of extension). &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;As &lt;/del&gt;the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;tend &lt;/del&gt;to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;affix &lt;/del&gt;downwards onto a single strand in basement, the geometry has led to those being termed flower construction. Fault zones with dominantly reverse faulting are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;often &lt;/del&gt;known as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/del&gt;flowers, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;whereas those &lt;/del&gt;with dominantly normal offsets are generally known as damaging flowers. The identification of such buildings, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;notably &lt;/del&gt;where &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;adverse &lt;/del&gt;flowers are developed on different segments of the same fault, are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;thought to be dependable &lt;/del&gt;indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes occur at the stepover areas of faults, forming lens-formed close to parallel arrays of horses. These &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;happen &lt;/del&gt;between two or more &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;massive &lt;/del&gt;bounding faults which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;normally &lt;/del&gt;have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;massive &lt;/del&gt;displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;only &lt;/del&gt;horizontal movement, thus there is no &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;such thing as a &lt;/del&gt;change in topography &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;on account &lt;/del&gt;of movement of the fault. In actuality, as strike-slip faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;develop into large &lt;/del&gt;and developed, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://wiki.die-karte-bitte.de/index.php/Benutzer_Diskussion:Latia59N7497205 durable garden trimmer] &lt;/del&gt;their &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;behavior changes &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [https://j2v.co.kr/bbs/board.php?bo_table=qa&amp;amp;wr_id=1017260 durable garden trimmer] &lt;/del&gt;becomes extra &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;advanced&lt;/del&gt;. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;A protracted &lt;/del&gt;strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;follow &lt;/del&gt;the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;principle &lt;/del&gt;fault path. These sub-parallel stretches are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;isolated &lt;/del&gt;by offsets at first, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;however &lt;/del&gt;over &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lengthy durations &lt;/del&gt;of time, they &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;will become &lt;/del&gt;related by stepovers to accommodate the strike-slip displacement. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;long &lt;/del&gt;stretches of strike-slip, the fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;airplane &lt;/del&gt;can start to curve, giving rise to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructions much like &lt;/del&gt;step overs. Right lateral &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/del&gt;of a strike-slip fault at a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;proper &lt;/del&gt;stepover (or overstep) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;offers &lt;/del&gt;rise to extensional bends characterised by zones of subsidence, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://knowledge.thinkingstorm.com/UserProfile/tabid/57/userId/1959598/Default.aspx durable garden trimmer] &lt;/del&gt;local normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;kind &lt;/ins&gt;of tectonics that is dominated by lateral (horizontal) movements &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/ins&gt;the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/ins&gt;the boundary between two tectonic plates, this is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/ins&gt;a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/ins&gt;or conservative plate boundary. Areas of strike-slip tectonics are characterised by particular deformation &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/ins&gt;together with: stepovers, Riedel &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[https://wiki.dulovic.tech/index.php/User:BrandieMrt Wood Ranger Power Shears website]&lt;/ins&gt;, flower buildings and strike-slip duplexes. Where the displacement alongside a zone of strike-slip deviates from parallelism with the zone itself, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;fashion &lt;/ins&gt;turns into both transpressional or transtensional relying on the sense of deviation. Strike-slip tectonics is characteristic of a number of geological environments, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://www.vokipedia.de/index.php?title=Forms_Of_Pruning_Shears Wood Ranger Power Shears website] together with &lt;/ins&gt;oceanic and continental &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;rework &lt;/ins&gt;faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sometimes form &lt;/ins&gt;as a number of separate fault segments which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;might be &lt;/ins&gt;offset from one another. The areas between the ends of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;adjoining &lt;/ins&gt;segments are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;generally known &lt;/ins&gt;as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;In the case of a dextral fault zone, a right-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/ins&gt;an extensional stepover as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement &lt;/ins&gt;on the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;two &lt;/ins&gt;segments leads to extensional deformation in the zone of offset, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;while &lt;/ins&gt;a left-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/ins&gt;a compressional stepover. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;lively &lt;/ins&gt;strike-slip techniques, earthquake ruptures &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;may &lt;/ins&gt;bounce from one &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;segment &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a different &lt;/ins&gt;across the intervening stepover, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://wiki.laduni.id/Quantifying_The_Impact_Of_Detection_Bias_From_Blended_Galaxies_On_Cosmic_Shear_Surveys Wood Ranger Power Shears coupon] [https://www.yewiki.org/Quality_Used_Machinery Wood Ranger Power Shears price] [http://classicalmusicmp3freedownload.com/ja/index.php?title=Best_Hairdressing_Scissors_2025:_Classic_Scissors_And_Thinning_Shears_For_A_Salon-High_Quality_Cut_At_Home buy Wood Ranger Power Shears] [https://www.koklek.go.th/question/welcome-to-recycling-equipment-corporation/ Wood Ranger Power Shears order now] order now &lt;/ins&gt;if the offset isn't too great. Numerical modelling has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instructed &lt;/ins&gt;that jumps of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a minimum of &lt;/ins&gt;eight km, or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;possibly more &lt;/ins&gt;are feasible. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;This &lt;/ins&gt;is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;more &lt;/ins&gt;than 10 km &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/ins&gt;an extensional stepover. The presence of stepovers &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;through &lt;/ins&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) throughout earthquake rupture. In the early levels of strike-slip fault formation, displacement within basement rocks produces characteristic fault constructions inside the overlying cover.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;This &lt;/ins&gt;will &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;also &lt;/ins&gt;be the case the place an &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;active &lt;/ins&gt;strike-slip zone lies inside an &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;space &lt;/ins&gt;of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;persevering with &lt;/ins&gt;sedimentation. At low levels of pressure, the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;general simple &lt;/ins&gt;shear causes a set of small faults to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;type&lt;/ins&gt;. The dominant set, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;often &lt;/ins&gt;known as R &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;shears&lt;/ins&gt;, types at about 15° to the underlying fault with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;identical &lt;/ins&gt;shear sense. The R shears are then linked by a second set, the R' shears, that kinds at about 75° to the principle fault trace. These two fault orientations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;can &lt;/ins&gt;be understood as conjugate fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;units &lt;/ins&gt;at 30° to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;brief &lt;/ins&gt;axis of the instantaneous pressure ellipse related to the straightforward shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;pressure &lt;/ins&gt;subject &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;attributable to &lt;/ins&gt;the displacements &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;utilized &lt;/ins&gt;at the bottom of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/ins&gt;sequence. With additional displacement, the Riedel fault segments will &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;are inclined &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;develop &lt;/ins&gt;into &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;absolutely &lt;/ins&gt;linked &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;till &lt;/ins&gt;a throughgoing fault is formed. The linkage typically happens with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;event &lt;/ins&gt;of a further set of shears &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;generally known as &lt;/ins&gt;'P &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;[http://viss.net.cn:3000/rhysellwood037 Wood Ranger Power Shears sale]&lt;/ins&gt;', that are roughly symmetrical to the R shears relative to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;overall &lt;/ins&gt;shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;path&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;somewhat &lt;/ins&gt;oblique segments will hyperlink downwards into the fault at the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;base &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/ins&gt;sequence with a helicoidal geometry. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Intimately&lt;/ins&gt;, many strike-slip faults at surface &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;encompass &lt;/ins&gt;en echelon or braided segments, which in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;many &lt;/ins&gt;instances were &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;most likely &lt;/ins&gt;inherited from &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/ins&gt;formed Riedel shears. In cross-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;part&lt;/ins&gt;, the displacements are dominantly reverse or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;normal &lt;/ins&gt;in kind depending on whether or not the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;overall &lt;/ins&gt;fault geometry is transpressional (i.e. with a small component of shortening) or transtensional (with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;part &lt;/ins&gt;of extension). &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Because &lt;/ins&gt;the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;have a tendency &lt;/ins&gt;to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;hitch &lt;/ins&gt;downwards onto a single strand in basement, the geometry has led to those being termed flower construction. Fault zones with dominantly reverse faulting are known as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;optimistic &lt;/ins&gt;flowers, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;while these &lt;/ins&gt;with dominantly normal offsets are generally known as damaging flowers. The identification of such buildings, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;particularly &lt;/ins&gt;where &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;optimistic &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;detrimental &lt;/ins&gt;flowers are developed on &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;totally &lt;/ins&gt;different segments of the same fault, are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;regarded as reliable &lt;/ins&gt;indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes occur at the stepover areas of faults, forming lens-formed close to parallel arrays of horses. These &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;occur &lt;/ins&gt;between two or more &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;large &lt;/ins&gt;bounding faults which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;usually &lt;/ins&gt;have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;large &lt;/ins&gt;displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;solely &lt;/ins&gt;horizontal movement, thus there is no change in topography &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;as a consequence &lt;/ins&gt;of movement of the fault. In actuality, as strike-slip faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;become giant &lt;/ins&gt;and developed, their &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;habits modifications &lt;/ins&gt;and becomes extra &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;complicated&lt;/ins&gt;. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;An extended &lt;/ins&gt;strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;comply with &lt;/ins&gt;the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;primary &lt;/ins&gt;fault path. These sub-parallel stretches are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;remoted &lt;/ins&gt;by offsets at first, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;but &lt;/ins&gt;over &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;long intervals &lt;/ins&gt;of time, they&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;'ll turn into &lt;/ins&gt;related by stepovers to accommodate the strike-slip displacement. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;lengthy &lt;/ins&gt;stretches of strike-slip, the fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;plane &lt;/ins&gt;can start to curve, giving rise to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;buildings similar to &lt;/ins&gt;step overs. Right lateral &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;motion &lt;/ins&gt;of a strike-slip fault at a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;right &lt;/ins&gt;stepover (or overstep) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;gives &lt;/ins&gt;rise to extensional bends characterised by zones of subsidence, local normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
		<author><name>CelsaWheeler08</name></author>	</entry>

	<entry>
		<id>http://www.vokipedia.de/index.php?title=In_Most_Zones_Of_Continent-continent_Collision&amp;diff=103681&amp;oldid=prev</id>
		<title>VitoStallcup88 am 16. August 2025 um 21:06 Uhr</title>
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				<updated>2025-08-16T21:06:22Z</updated>
		
		<summary type="html">&lt;p&gt;&lt;/p&gt;
&lt;table class='diff diff-contentalign-left'&gt;
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			&lt;td colspan='2' style=&quot;background-color: white; color:black;&quot;&gt;Version vom 16. August 2025, 21:06 Uhr&lt;/td&gt;
			&lt;/tr&gt;&lt;tr&gt;&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;
&lt;td colspan=&quot;2&quot; class=&quot;diff-lineno&quot;&gt;Zeile 1:&lt;/td&gt;&lt;/tr&gt;
&lt;tr&gt;&lt;td class='diff-marker'&gt;−&lt;/td&gt;&lt;td style=&quot;background: #ffa; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;kind &lt;/del&gt;of tectonics that&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;'s &lt;/del&gt;dominated by lateral (horizontal) movements inside the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/del&gt;the boundary between two tectonic plates, this is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/del&gt;a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/del&gt;or conservative plate boundary. Areas of strike-slip tectonics are characterised by &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;explicit &lt;/del&gt;deformation kinds together with: stepovers, Riedel shears, flower buildings and strike-slip duplexes. Where the displacement &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;along &lt;/del&gt;a zone of strike-slip deviates from parallelism with the zone itself,&amp;#160; [&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;git&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sparrowcomm.com/ulysseskessler Wood Ranger Power Shears website] [https://www.s&lt;/del&gt;-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shot&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;ru&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;forum//profile&lt;/del&gt;.php&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;?id=6277 Wood Ranger Power Shears website] [http:&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;/blueroses.top:8888/mikeldashwood3 Wood Ranger Power &lt;/del&gt;Shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;specs&lt;/del&gt;] &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Shears USA the model turns into both transpressional or &lt;/del&gt;transtensional relying on the sense of deviation. Strike-slip tectonics is characteristic of a number of geological environments, including oceanic and continental &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;remodel &lt;/del&gt;faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;sometimes kind &lt;/del&gt;as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;several &lt;/del&gt;separate fault segments which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;might be &lt;/del&gt;offset from one another. The areas between the ends of adjacent segments are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;often known &lt;/del&gt;as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Within &lt;/del&gt;the case of a dextral fault zone,&amp;#160; [https://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;andyfreund&lt;/del&gt;.de&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;/wiki&lt;/del&gt;/index.php?title=&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;What_Happens_To_Weapons_Confiscated_On_The_Airport Wood Ranger Power Shears shop&lt;/del&gt;] a right-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/del&gt;an extensional stepover as motion on the 2 segments leads to extensional deformation &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;within &lt;/del&gt;the zone of offset, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;while &lt;/del&gt;a left-stepping offset is &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;named &lt;/del&gt;a compressional stepover. For &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lively &lt;/del&gt;strike-slip &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;methods&lt;/del&gt;, earthquake ruptures &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;may jump &lt;/del&gt;from one &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;segment &lt;/del&gt;to another &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/del&gt;the intervening stepover, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt; [http://www.vokipedia.de/index.php?title=Benutzer:GretaMcAdam6925 Wood Ranger Power Shears shop] &lt;/del&gt;if the offset &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;will not be &lt;/del&gt;too &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;nice&lt;/del&gt;. Numerical modelling has recommended that jumps of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;at least &lt;/del&gt;eight km, or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;possibly &lt;/del&gt;extra are feasible. That is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;more &lt;/del&gt;than 10 km throughout an extensional stepover. The presence of stepovers &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;during &lt;/del&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;during &lt;/del&gt;earthquake rupture. &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;Within &lt;/del&gt;the early &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;phases &lt;/del&gt;of strike-slip fault formation, displacement within basement rocks produces characteristic fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;buildings within &lt;/del&gt;the overlying &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cowl&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;This can &lt;/del&gt;even be the case the place an lively strike-slip zone lies inside an &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;space &lt;/del&gt;of continuing sedimentation. At low &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;ranges &lt;/del&gt;of pressure, the overall &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;simple &lt;/del&gt;shear causes a set of small faults to form. The dominant set, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;referred to &lt;/del&gt;as R [&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;https&lt;/del&gt;://&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;marketingme&lt;/del&gt;.&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/del&gt;/&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;wiki/Introducing_The_Wood_Ranger_Power_Shears:_The_Ultimate_Tool_For_Gardeners_And_Landscapers &lt;/del&gt;Wood Ranger Power Shears &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;shop&lt;/del&gt;], &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;forms &lt;/del&gt;at about 15° to the underlying fault with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;identical &lt;/del&gt;shear sense. The R shears are then linked by a second set, the R' &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;[https://gitea.zqll.top/rosettalangler wood &lt;/del&gt;shears&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;]&lt;/del&gt;, that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;varieties &lt;/del&gt;at about 75° to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;main &lt;/del&gt;fault trace. These two fault orientations &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;could &lt;/del&gt;be understood as conjugate fault sets at 30° to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;brief &lt;/del&gt;axis of the instantaneous pressure ellipse related to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;easy &lt;/del&gt;shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;pressure field attributable to &lt;/del&gt;the displacements applied at the bottom of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/del&gt;sequence. With &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;further &lt;/del&gt;displacement, the Riedel fault segments will tend to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;grow to be &lt;/del&gt;fully linked until a throughgoing fault is formed. The linkage &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;often &lt;/del&gt;happens with the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;event &lt;/del&gt;of a further set of shears often &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/del&gt;'P shears', &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;which &lt;/del&gt;are roughly symmetrical to the R shears relative to the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;overall &lt;/del&gt;shear &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;path&lt;/del&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The considerably oblique segments will hyperlink downwards into the fault at the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;base &lt;/del&gt;of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cover &lt;/del&gt;sequence with a helicoidal geometry. In detail, many strike-slip faults at surface &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;consist of &lt;/del&gt;en echelon or braided segments, which in lots of &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;cases had been most likely &lt;/del&gt;inherited from &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;previously &lt;/del&gt;formed Riedel shears. In cross-&lt;del class=&quot;diffchange diffchange-inline&quot;&gt;part&lt;/del&gt;, the displacements are dominantly reverse or regular in &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;type relying &lt;/del&gt;on whether or not the general fault geometry is transpressional (i.e. with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;element &lt;/del&gt;of shortening) or transtensional (with a small &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;part &lt;/del&gt;of extension). As the faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;have a tendency &lt;/del&gt;to affix downwards onto a single strand in basement, the geometry has led to &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;these &lt;/del&gt;being termed flower construction. Fault zones with dominantly reverse faulting are often &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/del&gt;constructive flowers, whereas &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;these &lt;/del&gt;with dominantly &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;regular &lt;/del&gt;offsets are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;often &lt;/del&gt;known as &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;detrimental &lt;/del&gt;flowers. The identification of such &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;constructions&lt;/del&gt;, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;significantly &lt;/del&gt;where &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;positive &lt;/del&gt;and &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;unfavourable &lt;/del&gt;flowers are developed on &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;totally &lt;/del&gt;different segments of the &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;identical &lt;/del&gt;fault, are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;considered reliable &lt;/del&gt;indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes occur at the stepover areas of faults, forming lens-formed close to parallel arrays of horses. These &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;occur &lt;/del&gt;between two or &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;extra giant &lt;/del&gt;bounding faults which &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;usually &lt;/del&gt;have &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;giant &lt;/del&gt;displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;solely &lt;/del&gt;horizontal &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;motion&lt;/del&gt;, thus there &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;isn't any &lt;/del&gt;change in topography &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;attributable to motion &lt;/del&gt;of the fault. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;reality&lt;/del&gt;, as strike-slip faults &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;grow to be massive &lt;/del&gt;and developed, their behavior changes and becomes extra &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;complex&lt;/del&gt;. A protracted strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;comply with &lt;/del&gt;the principle fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;route&lt;/del&gt;. These sub-parallel stretches are &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;remoted &lt;/del&gt;by offsets at first, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;but &lt;/del&gt;over &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;long intervals &lt;/del&gt;of time, they will &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;develop into linked &lt;/del&gt;by stepovers to accommodate the strike-slip displacement. In &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;lengthy &lt;/del&gt;stretches of strike-slip, the fault &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;plane &lt;/del&gt;can &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;begin &lt;/del&gt;to curve, giving rise to constructions &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;just &lt;/del&gt;like step overs. Right lateral movement of a strike-slip fault at a &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;right &lt;/del&gt;stepover (or overstep) &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;provides &lt;/del&gt;rise to extensional bends characterised by zones of subsidence, &lt;del class=&quot;diffchange diffchange-inline&quot;&gt;native &lt;/del&gt;normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;td class='diff-marker'&gt;+&lt;/td&gt;&lt;td style=&quot;background: #cfc; color:black; font-size: smaller;&quot;&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sort &lt;/ins&gt;of tectonics that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is &lt;/ins&gt;dominated by lateral (horizontal) movements inside the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;forms &lt;/ins&gt;the boundary between two tectonic plates, this is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/ins&gt;a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;remodel &lt;/ins&gt;or conservative plate boundary. Areas of strike-slip tectonics are characterised by &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;particular &lt;/ins&gt;deformation kinds together with: stepovers, Riedel shears, flower buildings and strike-slip duplexes. Where the displacement &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;alongside &lt;/ins&gt;a zone of strike-slip deviates from parallelism with the zone itself, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;the model turns into both transpressional or &lt;/ins&gt; [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;wiki&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;die-karte&lt;/ins&gt;-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;bitte&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;de&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;index&lt;/ins&gt;.php/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Professional_Garden_Tools-Premium_Bypass_Pruners-&lt;/ins&gt;Shears &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;durable garden trimmer&lt;/ins&gt;] transtensional relying on the sense of deviation. Strike-slip tectonics is characteristic of a number of geological environments, including oceanic and continental &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;transform &lt;/ins&gt;faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;usually type &lt;/ins&gt;as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;a number of &lt;/ins&gt;separate fault segments which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;are &lt;/ins&gt;offset from one another. The areas between the ends of adjacent segments are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;referred to &lt;/ins&gt;as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;In &lt;/ins&gt;the case of a dextral fault zone,&amp;#160; [https://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;systemcheck-wiki&lt;/ins&gt;.de/index.php?title=&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;Easy_Methods_To_Make_Shears_In_Minecraft durable garden trimmer&lt;/ins&gt;] a right-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/ins&gt;an extensional stepover as motion on the 2 segments leads to extensional deformation &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;in &lt;/ins&gt;the zone of offset, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;whereas &lt;/ins&gt;a left-stepping offset is &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/ins&gt;a compressional stepover. For &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;energetic &lt;/ins&gt;strike-slip &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;techniques&lt;/ins&gt;, earthquake ruptures &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;could bounce &lt;/ins&gt;from one &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;phase &lt;/ins&gt;to another &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;across &lt;/ins&gt;the intervening stepover, if the offset &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;just isn't &lt;/ins&gt;too &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;great&lt;/ins&gt;. Numerical modelling has recommended that jumps of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;not less than &lt;/ins&gt;eight km, or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;presumably &lt;/ins&gt;extra are feasible. That is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;greater &lt;/ins&gt;than 10 km throughout an extensional stepover. The presence of stepovers &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;throughout &lt;/ins&gt;earthquake rupture. &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;In &lt;/ins&gt;the early &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;levels &lt;/ins&gt;of strike-slip fault formation, displacement within basement rocks produces characteristic fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constructions inside &lt;/ins&gt;the overlying &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cover&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;It will &lt;/ins&gt;even be the case the place an lively strike-slip zone lies inside an &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;area &lt;/ins&gt;of continuing sedimentation. At low &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;levels &lt;/ins&gt;of pressure, the overall &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;easy &lt;/ins&gt;shear causes a set of small faults to form. The dominant set, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;generally known &lt;/ins&gt;as R [&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;http&lt;/ins&gt;://&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;sinzero&lt;/ins&gt;.&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;xyz:3000&lt;/ins&gt;/&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;martyits143965 buy &lt;/ins&gt;Wood Ranger Power Shears], &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;types &lt;/ins&gt;at about 15° to the underlying fault with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;same &lt;/ins&gt;shear sense. The R shears are then linked by a second set, the R' shears, that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;kinds &lt;/ins&gt;at about 75° to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;principle &lt;/ins&gt;fault trace. These two fault orientations &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;will &lt;/ins&gt;be understood as conjugate fault sets at 30° to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;quick &lt;/ins&gt;axis of the instantaneous pressure ellipse related to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;straightforward &lt;/ins&gt;shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;strain subject caused by &lt;/ins&gt;the displacements applied at the bottom of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/ins&gt;sequence. With &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;additional &lt;/ins&gt;displacement, the Riedel fault segments will tend to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;change into &lt;/ins&gt;fully linked until a throughgoing fault is formed. The linkage &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;typically &lt;/ins&gt;happens with the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;development &lt;/ins&gt;of a further set of shears often &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;called &lt;/ins&gt;'P shears', &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;that &lt;/ins&gt;are roughly symmetrical to the R shears relative to the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;general &lt;/ins&gt;shear &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;course&lt;/ins&gt;.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The considerably oblique segments will hyperlink downwards into the fault at the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;bottom &lt;/ins&gt;of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;cowl &lt;/ins&gt;sequence with a helicoidal geometry. In detail, many strike-slip faults at surface &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;include &lt;/ins&gt;en echelon or braided segments, which in lots of &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;instances were in all probability &lt;/ins&gt;inherited from &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;beforehand &lt;/ins&gt;formed Riedel shears. In cross-&lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;section&lt;/ins&gt;, the displacements are dominantly reverse or regular in &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;kind depending &lt;/ins&gt;on whether or not the general fault geometry is transpressional (i.e. with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;component &lt;/ins&gt;of shortening) or transtensional (with a small &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;element &lt;/ins&gt;of extension). As the faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;tend &lt;/ins&gt;to affix downwards onto a single strand in basement, the geometry has led to &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;those &lt;/ins&gt;being termed flower construction. Fault zones with dominantly reverse faulting are often &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;known as &lt;/ins&gt;constructive flowers, whereas &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;those &lt;/ins&gt;with dominantly &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;normal &lt;/ins&gt;offsets are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;generally &lt;/ins&gt;known as &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;damaging &lt;/ins&gt;flowers. The identification of such &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;buildings&lt;/ins&gt;, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;notably &lt;/ins&gt;where &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;constructive &lt;/ins&gt;and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;adverse &lt;/ins&gt;flowers are developed on different segments of the &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;same &lt;/ins&gt;fault, are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;thought to be dependable &lt;/ins&gt;indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes occur at the stepover areas of faults, forming lens-formed close to parallel arrays of horses. These &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;happen &lt;/ins&gt;between two or &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;more massive &lt;/ins&gt;bounding faults which &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;normally &lt;/ins&gt;have &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;massive &lt;/ins&gt;displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;only &lt;/ins&gt;horizontal &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;movement&lt;/ins&gt;, thus there &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;is no such thing as a &lt;/ins&gt;change in topography &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;on account of movement &lt;/ins&gt;of the fault. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;actuality&lt;/ins&gt;, as strike-slip faults &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;develop into large &lt;/ins&gt;and developed, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://wiki.die-karte-bitte.de/index.php/Benutzer_Diskussion:Latia59N7497205 durable garden trimmer] &lt;/ins&gt;their behavior changes and &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [https://j2v.co.kr/bbs/board.php?bo_table=qa&amp;amp;wr_id=1017260 durable garden trimmer] &lt;/ins&gt;becomes extra &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;advanced&lt;/ins&gt;. A protracted strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;follow &lt;/ins&gt;the principle fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;path&lt;/ins&gt;. These sub-parallel stretches are &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;isolated &lt;/ins&gt;by offsets at first, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;however &lt;/ins&gt;over &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;lengthy durations &lt;/ins&gt;of time, they will &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;become related &lt;/ins&gt;by stepovers to accommodate the strike-slip displacement. In &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;long &lt;/ins&gt;stretches of strike-slip, the fault &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;airplane &lt;/ins&gt;can &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;start &lt;/ins&gt;to curve, giving rise to constructions &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;much &lt;/ins&gt;like step overs. Right lateral movement of a strike-slip fault at a &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;proper &lt;/ins&gt;stepover (or overstep) &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt;offers &lt;/ins&gt;rise to extensional bends characterised by zones of subsidence, &lt;ins class=&quot;diffchange diffchange-inline&quot;&gt; [http://knowledge.thinkingstorm.com/UserProfile/tabid/57/userId/1959598/Default.aspx durable garden trimmer] local &lt;/ins&gt;normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;&lt;/td&gt;&lt;/tr&gt;
&lt;/table&gt;</summary>
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		<title>GretaMcAdam6925: Die Seite wurde neu angelegt: „&lt;br&gt;Strike-slip tectonics or wrench tectonics is a kind of tectonics that's dominated by lateral (horizontal) movements inside the Earth's crust (and lithosphe…“</title>
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		<summary type="html">&lt;p&gt;Die Seite wurde neu angelegt: „&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a kind of tectonics that&amp;#039;s dominated by lateral (horizontal) movements inside the Earth&amp;#039;s crust (and lithosphe…“&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Neue Seite&lt;/b&gt;&lt;/p&gt;&lt;div&gt;&amp;lt;br&amp;gt;Strike-slip tectonics or wrench tectonics is a kind of tectonics that's dominated by lateral (horizontal) movements inside the Earth's crust (and lithosphere). Where a zone of strike-slip tectonics types the boundary between two tectonic plates, this is named a transform or conservative plate boundary. Areas of strike-slip tectonics are characterised by explicit deformation kinds together with: stepovers, Riedel shears, flower buildings and strike-slip duplexes. Where the displacement along a zone of strike-slip deviates from parallelism with the zone itself,  [https://git.sparrowcomm.com/ulysseskessler Wood Ranger Power Shears website] [https://www.s-shot.ru/forum//profile.php?id=6277 Wood Ranger Power Shears website] [http://blueroses.top:8888/mikeldashwood3 Wood Ranger Power Shears specs] Shears USA the model turns into both transpressional or transtensional relying on the sense of deviation. Strike-slip tectonics is characteristic of a number of geological environments, including oceanic and continental remodel faults, zones of oblique collision and the deforming foreland of zones of continental collision. When strike-slip fault zones develop, they sometimes kind as several separate fault segments which might be offset from one another. The areas between the ends of adjacent segments are often known as stepovers.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Within the case of a dextral fault zone,  [https://andyfreund.de/wiki/index.php?title=What_Happens_To_Weapons_Confiscated_On_The_Airport Wood Ranger Power Shears shop] a right-stepping offset is named an extensional stepover as motion on the 2 segments leads to extensional deformation within the zone of offset, while a left-stepping offset is named a compressional stepover. For lively strike-slip methods, earthquake ruptures may jump from one segment to another throughout the intervening stepover,  [http://www.vokipedia.de/index.php?title=Benutzer:GretaMcAdam6925 Wood Ranger Power Shears shop] if the offset will not be too nice. Numerical modelling has recommended that jumps of at least eight km, or possibly extra are feasible. That is backed up by evidence that the rupture of the 2001 Kunlun earthquake jumped more than 10 km throughout an extensional stepover. The presence of stepovers during the rupture of strike-slip fault zones has been related to the initiation of supershear propagation (propagation in excess of the S wave velocity) during earthquake rupture. Within the early phases of strike-slip fault formation, displacement within basement rocks produces characteristic fault buildings within the overlying cowl.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;This can even be the case the place an lively strike-slip zone lies inside an space of continuing sedimentation. At low ranges of pressure, the overall simple shear causes a set of small faults to form. The dominant set, referred to as R [https://marketingme.wiki/wiki/Introducing_The_Wood_Ranger_Power_Shears:_The_Ultimate_Tool_For_Gardeners_And_Landscapers Wood Ranger Power Shears shop], forms at about 15° to the underlying fault with the identical shear sense. The R shears are then linked by a second set, the R' [https://gitea.zqll.top/rosettalangler wood shears], that varieties at about 75° to the main fault trace. These two fault orientations could be understood as conjugate fault sets at 30° to the brief axis of the instantaneous pressure ellipse related to the easy shear pressure field attributable to the displacements applied at the bottom of the cover sequence. With further displacement, the Riedel fault segments will tend to grow to be fully linked until a throughgoing fault is formed. The linkage often happens with the event of a further set of shears often known as 'P shears', which are roughly symmetrical to the R shears relative to the overall shear path.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;The considerably oblique segments will hyperlink downwards into the fault at the base of the cover sequence with a helicoidal geometry. In detail, many strike-slip faults at surface consist of en echelon or braided segments, which in lots of cases had been most likely inherited from previously formed Riedel shears. In cross-part, the displacements are dominantly reverse or regular in type relying on whether or not the general fault geometry is transpressional (i.e. with a small element of shortening) or transtensional (with a small part of extension). As the faults have a tendency to affix downwards onto a single strand in basement, the geometry has led to these being termed flower construction. Fault zones with dominantly reverse faulting are often called constructive flowers, whereas these with dominantly regular offsets are often known as detrimental flowers. The identification of such constructions, significantly where positive and unfavourable flowers are developed on totally different segments of the identical fault, are considered reliable indicators of strike-slip.&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;&amp;lt;br&amp;gt;Strike-slip duplexes occur at the stepover areas of faults, forming lens-formed close to parallel arrays of horses. These occur between two or extra giant bounding faults which usually have giant displacements. An idealized strike-slip fault runs in a straight line with a vertical dip and has solely horizontal motion, thus there isn't any change in topography attributable to motion of the fault. In reality, as strike-slip faults grow to be massive and developed, their behavior changes and becomes extra complex. A protracted strike-slip fault follows a staircase-like trajectory consisting of interspaced fault planes that comply with the principle fault route. These sub-parallel stretches are remoted by offsets at first, but over long intervals of time, they will develop into linked by stepovers to accommodate the strike-slip displacement. In lengthy stretches of strike-slip, the fault plane can begin to curve, giving rise to constructions just like step overs. Right lateral movement of a strike-slip fault at a right stepover (or overstep) provides rise to extensional bends characterised by zones of subsidence, native normal faults, and pull-apart basins.&amp;lt;br&amp;gt;&lt;/div&gt;</summary>
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