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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Paleoseismic Investigation of the Aksay Restraining Double Bend, Altyn Tagh Fault, and Its Implication for Barrier‐Breaching Ruptures
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Paleoseismic Investigation of the Aksay Restraining Double Bend, Altyn Tagh Fault, and Its Implication for Barrier‐Breaching Ruptures

机译：Aksay抑制双重弯曲，Altyn Tagh故障的古半发作调查及其对障碍破裂的影响

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Abstract >Fault geometry is recognized as an important control on earthquake rupture extent, magnitude, and recurrence behavior. However, multicycle earthquake rupture simulations indicate that geometrical barriers do not always stop rupture propagation. Stress buildup over multiple prior earthquakes may promote an occasional breach of a barrier, producing a significantly larger rupture. Here we present paleoseismic data from the Aksay restraining double bend of the Altyn Tagh fault, which supports such breaching. The Aksay bend consists of two main strands, which bend together in a broad transpressional configuration. We investigate the paleo‐earthquake histories of both strands to assess the correlation of events within and beyond the bend. The south strand exhibits four very likely paleo‐earthquakes with an average interval of 1,433?±?57?years and a coefficient of variation (COV) of ~ 0.5. The north strand records four highest‐quality events after 3650?Before Common Era with an average interval of ~1,326?±?179?years and a COV of ~0.3. The varying recurrence intervals and relatively high COVs indicate that faults within the Aksay bend have only quasi‐periodic rupture recurrence. Comparing the event sequences also suggests a complex rupture history. The penultimate event appears to correlate across the bend, as well as to previously published paleoseismic chronologies both to the east and to the west, which supports it being a barrier‐breaching event. The event histories reported here indicate that multiple earthquakes must terminate within the bend, over several earthquake cycles, in order to arrive at a stress condition suitable for a breaching earthquake rupture. </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 Type =“Main”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >故障几何体被识别为地震破裂程度，幅度和复发行为的重要控制。然而，多运行地震破裂模拟表明几何屏障并不总是停止破裂的传播。在多次现有地震上的压力积聚可能会促进禁止障碍的禁用，产生显着更大的破裂。在这里，我们从Aksay抑制Akyn Tagh故障的双重弯曲的Aksay造成古摆力，这支持了这种突发。 Aksay弯曲由两个主要股线组成，该主股在一起以广泛的压碎配置弯曲。我们调查两条股的古地震历史，以评估弯曲内外事件的相关性。南股展示了四个很可能的古地地震，平均间隔为1,433？±57？年和变异系数（COV）〜0.5。在3650后，北股记录了四个最高质量的事件？在普通时代之前，平均间隔〜1,326？±179？年和一个0.3的COV。不同的复发间隔和相对高的COV表示，Aksay弯曲内的故障仅具有准周期性破裂复发。比较事件序列也表明了复杂的破裂历史。倒数第二个事件似乎与弯曲有关，以及以前发表过的东部和西部的古摆态度，这支持它是一个障碍违规事件。这里报道的事件历史表明，多次地震必须在弯曲内终止于几个地震循环，以便到达适合突破地震破裂的应力条件。</ p> </摘要> </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>2018年第5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=Shao Yanxiu&option=202" target="_blank" rel="nofollow">Shao Yanxiu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu‐Zeng Jing&option=202" target="_blank" rel="nofollow">Liu‐Zeng Jing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oskin Michael E.&option=202" target="_blank" rel="nofollow">Oskin Michael E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Elliott Austin J.&option=202" target="_blank" rel="nofollow">Elliott Austin J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Peng&option=202" target="_blank" rel="nofollow">Wang Peng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Jinyu&option=202" target="_blank" rel="nofollow">Zhang Jinyu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yuan Zhaode&option=202" target="_blank" rel="nofollow">Yuan Zhaode;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Zhanfei&option=202" target="_blank" rel="nofollow">Li Zhanfei;</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>State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>Department of Earth and Planetary SciencesUniversity of CaliforniaDavis CA USA;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>State Key Laboratory of Earthquake Dynamics Institute of GeologyChina Earthquake AdministrationBeijing China;</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=Altyn Tagh fault&option=203" rel="nofollow">Altyn Tagh fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=the Aksay restraining double bend&option=203" rel="nofollow">the Aksay restraining double bend;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleoseismology&option=203" rel="nofollow">paleoseismology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fault geometry&option=203" rel="nofollow">fault geometry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake recurrence behavior&option=203" rel="nofollow">earthquake recurrence behavior;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake cycle&option=203" rel="nofollow">earthquake cycle;</a> </p> <div class="translation"> 机译：ALTYN TAGH故障;aksay抑制双弯;古摆力;断层几何;地震复发行为;地震周期; 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