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What can strike‐slip fault spacing tell us about the plate boundary of western North America?

机译：什么可以击打故障间距告诉我们北美西部的板材边界？

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Abstract > The spacing of parallel continental strike‐slip faults can constrain the mechanical properties of the faults and fault‐bounded crust. In the western <fc>US</fc> , evenly spaced strike‐slip fault domains are observed in the San Andreas ( <fc>SA</fc> ) and Walker Lane ( <fc>WL</fc> ) fault systems. Comparison of fault spacing ( S ) vs. seismogenic zone thickness ( L ) relationships of the <fc>SA</fc> and <fc>WL</fc> systems indicates that the <fc>SA</fc> has a higher S / L ratio (~8 vs. 1, respectively). If a stress‐shadow mechanism guides parallel fault formation, the S / L ratio should be controlled by fault strength, crustal strength, and/or regional stress. This suggests that the <fc>SA</fc> ‐related strike‐slip faults are relatively weaker, with lower fault friction: 0.13–0.19 for the <fc>SA</fc> vs. 0.20 for <fc>WL</fc> . The observed mechanical differences between the San Andreas and Walker Lane fault systems may be attributed to variations in the local geology of the fault‐hosting crust and/or the regional boundary conditions (e.g. geothermal gradient or strain rate). </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract XMLNS =“http://www.wiley.com/namespaces/wiley”type =“main”xml：id =“ter12315-abs-0001”xml：lang =“en”> <标题类型=“main” >摘要</ title> >并行大陆击破故障的间距可以限制故障的机械性能和故障有界外壳。在Western <Fc> US </ FC>中，在San Andreas（<FC> SA </ FC>）和Walker Lane（<FC> WL </ FC>）故障系统中观察到均匀间隔的防滑故障域。 <FC> SA </ FC>和<FC> WL </ FC>系统的发生故障间距（ s </ i>）与脱模区厚度（ l </ i>）关系的比较表示<FC> SA </ FC>具有较高的 s </ i> / l </ i>比率（分别为〜8 vs.1）。如果应激阴影机构引导平行故障形成，则应通过故障强度，地壳强度和/或区域应力来控制I> S </ i> / L </ i>。这表明<FC> SA </ FC> - 相关的防滑故障是相对较弱的，具有较低的故障摩擦：<FC> SA </ FC>的0.13-0.19 <FC> WL </ FC>。 San Andreas和Walker Lane故障系统之间观察到的机械差异可能归因于故障托管地壳和/或区域边界条件的局部地质的变化（例如地热梯度或应变率）。 </ p> </ abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-30393/'>《Terra Nova》</a> <b style="margin: 0 2px;">|</b><span>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共9页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zuza Andrew V.&option=202" target="_blank" rel="nofollow">Zuza Andrew V.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carlson Chad W.&option=202" target="_blank" rel="nofollow">Carlson Chad W.;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>Nevada Bureau of Mines and GeologyUniversity of NevadaReno NV USA;</p> <p>Nevada Bureau of Mines and GeologyUniversity of NevadaReno NV USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/14.html" title="天文学、地球科学">天文学、地球科学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> </p> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024722653.html">What can strike‐slip fault spacing tell us about the plate boundary of western North America?</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zuza Andrew V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zuza Andrew V.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carlson Chad W.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Carlson Chad W. </a> <a href="/journal-foreign-30393/" target="_blank" rel="nofollow" class="tuijian_authcolor">Terra Nova .</a> <span>2018</span><span>,第2期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：什么可以击打故障间距告诉我们北美西部的板材边界？</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_geotectonics_thesis/0204112287317.html">Strike-slip fault system in the Earth's crust of the Bering Sea: A relic of boundary between the Eurasian and North American lithospheric plates</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chekhovich V. 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