Paleomagnetic Rotation Constraints on the Deformation of the Northern Qaidam Marginal Thrust Belt and Implications for Strike‐Slip Faulting Along the Altyn Tagh Fault

Li Bingshuai; Yan Maodu; Zhang Weilin; Fang Xiaomin; Yang Yongpeng; Zhang Dawen; Chen Yi; Guan Chong

摘要

Abstract >Discordant Cenozoic paleomagnetic rotation results obtained throughout the northeastern Tibetan Plateau have yielded different tectonic models for the evolution of the Altyn Tagh Fault and the northeastern Tibetan Plateau. Here based on detailed existing magnetostratigraphic age constraints, we carried out an in‐depth paleomagnetic study along the Hongliugou section in the middle northern Qaidam marginal thrust belt to address the Cenozoic rotations of this region. A total of 1,342 Jurassic‐Neogene siltstone‐sandstone core samples were collected from 128 sites across 18 time intervals. Rock magnetic analysis suggested that magnetite and hematite are the dominant magnetic carriers. Detailed thermal demagnetization analyses were performed, and the characteristic remanent magnetizations of 90 sites (743 samples) were obtained, which yielded positive fold and reversals tests, indicating that they likely represent primary magnetizations. Detailed paleomagnetic declination versus age analyses revealed three periods of rotations: ~12.5?±?15.7° statistically insignificant counterclockwise rotations during ~45–33?Ma, successive clockwise rotations of ~32.2?±?15.4° during ~33–14?Ma, and subsequent statistically insignificant counterclockwise rotations of ~8.7?±?9.4° after ~14?Ma. These three periods of rotations are similar to those calculated based on previously available magnetostratigraphic data from the nearby Dahonggou section. Based on the integration of these data with other lines of geological evidence, we attributed the latter two periods of rotations to fast strike‐slip faulting along the Altyn Tagh Fault. </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</标题> >在东北藏高原地区均获得的不间断的新生代古磁性旋转结果为进化产生了不同的构造模型Altyn Tagh断层与东北高原东北部。在这里，基于详细的现有磁性数据造成寿命约束，我们沿着柴达木北部北部边缘止推皮带的洪欣口段进行了深入的古磁性研究，以解决该地区的新生代轮换。在18个时间间隔的128个位点收集了总共1,342个侏罗纪 - 新生氨基砂岩核心样品。岩石磁性分析表明，磁铁矿和赤铁矿是主要的磁性载体。进行了详细的热退磁分析，获得了90个位点（743个样品）的特征刚性磁化，从而产生正折叠和逆转试验，表明它们可能代表初级磁化。详细的古磁悬垂与年龄分析显示三个旋转时段：〜12.5？±15.7°统计学上逆时针旋转〜45-33？ma，连续顺时针旋转〜32.2？±15.4°期间〜33-14？随后的统计上微不足道的逆时针旋转〜8.7？±9.4°后〜14？ma。这三个旋转时段与基于来自附近的Dahonggou部分的先前可用的磁性数据数据计算的旋转期相似。根据这些数据与其他地质证据的集成，我们将后两段旋转归因于沿着ALTYN TAGH故障的快速防滑断层。</ 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9期</span><b style="margin: 0 2px;">|</b><span>共18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=Li Bingshuai&option=202" target="_blank" rel="nofollow">Li Bingshuai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Maodu&option=202" target="_blank" rel="nofollow">Yan Maodu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Weilin&option=202" target="_blank" rel="nofollow">Zhang Weilin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fang Xiaomin&option=202" target="_blank" rel="nofollow">Fang Xiaomin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Yongpeng&option=202" target="_blank" rel="nofollow">Yang Yongpeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Dawen&option=202" target="_blank" rel="nofollow">Zhang Dawen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Yi&option=202" target="_blank" rel="nofollow">Chen Yi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guan Chong&option=202" target="_blank" rel="nofollow">Guan Chong;</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>School of Earth SciencesEast China University of TechnologyNanchang China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 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=Cenozoic&option=203" rel="nofollow">Cenozoic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleomagnetic rotations&option=203" rel="nofollow">paleomagnetic rotations;</a> <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=northern Qaidam marginal thrust belt&option=203" rel="nofollow">northern Qaidam marginal thrust belt;</a> </p> <div class="translation"> 机译：新生代;古磁体旋转;阿莱恩Tagh故障;北柴达木北部边缘推力带; 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1997</span><span>,第005期</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130471754646.html">OBSERVATION SPACER FOR MEASURING OF EARTH STRIKE-SLIP FAULTS AS WELL AS ROCKS IN A WELL</a> <b>[P]</b> . <span> 外国专利：  CS242362B1 </span> <span> . 1986-04-17</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：测井地震走滑断裂以及岩石中的观测空间 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130455024937.html">Method and device for monitoring rotational speed sensors of vehicles for faults using a slip coefficient weighted by time</a> <b>[P]</b> . <span> 外国专利：  US5650718A </span> <span> . 1997-07-22</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：使用时间加权的滑移系数来监测车辆转速传感器故障的方法和装置 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130414805013.html">Magnetic drill pedestal mounting plate. Application: To secure a magnetic drill to the top of a pedestal for the purpose of drilling, or with machining applications. This provides a better drilling / machining method in contrast to a belt drive application, that has faults ie: slipping and lack of constant power and ease of access to variable speed selection, this device allows a magnetic drill to drill stainless steel and aluminium where normally a magnetic drill can't be mounted.</a> <b>[P]</b> . <span> 外国专利：  AU2014100971A4 </span> <span> . 2014-11-27</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：电磁钻基座安装板。应用：将磁钻固定在基座顶部以进行钻孔或用于机械加工。与皮带驱动应用相比，这提供了一种更好的钻孔/机加工方法，该应用具有以下缺点：滑移，缺乏恒定功率并且难以进行变速选择，该设备允许电磁钻在通常情况下在不锈钢和铝上钻孔无法安装电磁钻。 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" 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