Rapid Geodetic Shortening Across the Eastern Cordillera of NW Argentina Observed by the Puna‐Andes GPS Array

机译：普通GPS阵列观察到NW阿根廷东部Ceartern的快速大地缩短

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Abstract > We present crustal velocities for 29 continuously recording GPS stations from the southern central Andes across the Puna, Eastern Cordillera, and Santa Barbara system for the period between the 27 February 2010 Maule and 1 April 2014 Iquique earthquakes in a South American frame. The velocity field exhibits a systematic decrease in magnitude from ~35?mm/yr near the trench to 1?mm/yr within the craton. We forward model loading on the Nazca‐South America (NZ‐SA) subduction interface using back slip on elastic dislocations to approximate a fully locked interface from 10 to 50?km depth. We generate an ensemble of models by iterating over the percentage of NZ‐SA convergence accommodated at the subduction interface. Velocity residuals calculated for each model demonstrate that locking on the NZ‐SA interface is insufficient to reproduce the observed velocities. We model deformation associated with a back‐arc décollement using an edge dislocation, estimating model parameters from the velocity residuals for each forward model of the subduction interface ensemble using a Bayesian approach. We realize our best fit to the thrust‐perpendicular velocity field with type="mathematics">70?±?5% of NZ‐SA convergence accommodated at the subduction interface and a slip rate of type="mathematics">9.1?±?0.9 ?mm/yr on the fold‐thrust belt décollement. We also estimate a locking depth of type="mathematics">14?±?9 ?km, which places the downdip extent of the locked zone type="mathematics">135?±?20 ?km from the thrust front. The thrust‐parallel component of velocity is fit by a constant shear strain rate of ?19?×?10 ?9 ?yr ?1 , equivalent to clockwise rigid block rotation of the back arc at a rat </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 Type =“main”XML：lang =“en”> <标题类型=“main”>抽象</ title> >我们呈现出色速度29持续录制来自旁观南部的南部的GPS站，东部Cardillera和Santa Barbara系统在2010年2月27日的毛灵和2014年4月1日南美洲框架中的Iquique地震。速度场在沟槽附近的〜35Ωmm/ yr的幅度幅度幅度为1。我们在Nazca-South America（NZ-SA）俯冲界面上的模型加载使用弹性脱位对弹性脱模来近似从10到50的完全锁定的界面。我们通过迭代在俯冲界面处容纳的NZ-SA收敛百分比来生成模型的集合。针对每个模型计算的速度残差表明，在NZ-SA接口上锁定不足以再现观察到的速度。我们使用边缘位错，使用边缘位错，估计来自俯卧件的速度残差来估计模型参数的模型与俯卧的血管符合的速度差异使用贝叶斯方法。我们实现了最适合与<跨度=“数学”> 70？±5％</跨度>在俯视接口处的NZ-SA收敛和<跨度型=的滑动速率的速度贴合“数学”> 9.1？±0.9 </跨度>？折叠推力皮带中的毫米/毫秒。我们还估计<跨度类型=“数学”> 14的锁定深度> 14？±9 </ span>？km，它将锁定区域类型=“数学”> 135？±20 < /跨度>距离推力前面的人。速度的推力平行分量通过恒定的剪切应变速率为19？×10 Δ9</ sup>Δω1，相当于顺时针刚性块旋转在大鼠的后弧 </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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2017年第10期</span><b style="margin: 0 2px;">|</b><span>共24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=McFarland Phillip K.&option=202" target="_blank" rel="nofollow">McFarland Phillip K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bennett Richard A.&option=202" target="_blank" rel="nofollow">Bennett Richard A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alvarado Patricia&option=202" target="_blank" rel="nofollow">Alvarado Patricia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=DeCelles Peter G.&option=202" target="_blank" rel="nofollow">DeCelles Peter G.;</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>Department of GeosciencesUniversity of ArizonaTucson AZ;</p> <p>Department of GeosciencesUniversity of ArizonaTucson AZ;</p> <p>Departamento de Geofisica y AstronomíaFCEFN–Universidad Nacional de San JuanRivadavia Argentina;</p> <p>Department of GeosciencesUniversity of ArizonaTucson AZ;</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/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal deformation&option=203" rel="nofollow">crustal deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=central Andes&option=203" rel="nofollow">central Andes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geodesy&option=203" rel="nofollow">geodesy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=active tectonics&option=203" rel="nofollow">active tectonics;</a> </p> <div class="translation"> 机译：地壳变形;中央山脉;大地测量;积极构造; </div> </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704020651937.html">Rapid Geodetic Shortening Across the Eastern Cordillera of NW Argentina Observed by the Puna-Andes GPS Array</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McFarland Phillip K.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">McFarland Phillip K.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bennett Richard A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bennett Richard A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alvarado Patricia&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alvarado Patricia,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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