Oblique Thrusting and Strain Partitioning in the Longmen Shan Fold‐and‐Thrust Belt, Eastern Tibetan Plateau

机译：龙门山折叠带，东藏高原倾斜推进和应变分区

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Abstract > Eastern Tibet is an important example of oblique convergence and associated strain partitioning, as suggested by recent 2‐D and 3‐D structural interpretations, yet the nature and evolution of oblique strain partitioning of this region remain poorly known. Here we use seismic reflection profiles, borehole data, and field investigations in the Longmen Shan piedmont to determine the subsurface structural architecture, and we observe several nearly N‐S striking thrusts and reactivation of NE striking preexisting faults. We interpret that this behavior is due to a regional principal compressional stress oriented in the E‐W direction, oblique to the NE striking Longmen Shan. Using the records of fault activity and related Late Pliocene and Quaternary foreland sediments and growth strata, as well as the coseismic rupture of the 2008 M <sub> w </sub> 7.9 Wenchuan earthquake, we demonstrate that the Longmen Shan has experienced E‐W crustal shortening and oblique motion since ~5–2?Ma. We present two strain partitioning models arising from oblique thrusting in eastern Tibet and suggest that the eastward extrusion from Tibet is mainly accommodated on the strike‐slip Longriba fault and the dip‐slip Longmen Shan‐Min Shan fault zones. These results enhance our understanding of the tectonic relationship between the Songpan‐Ganzi terrane and the Sichuan basin and provide additional constraints for studies of the geodynamic response of eastern Tibet to the ongoing India‐Eurasia collision. </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> >东藏是倾斜融合和相关的应变分区的一个重要例子，如最近的2所提出的建议-D和3-D结构解释，然而，该地区倾斜应变分区的性质和演化仍然知名。在这里，我们使用地震反射型材，钻孔数据和龙门山皮埃蒙特的现场调查来确定地下结构架构，我们观察几乎几乎N-S醒目的推力并重新激活NE引人注目的预先存在的故障。我们解释了这种行为是由于E-W方向导向的区域主要压缩压力，倾斜地肆虐龙门山。利用故障活动和相关晚期基调和第四纪前陆沉积物和生长阶层的记录，以及2008年的电影症破裂 m w </ sub> 7.9汶川地震，我们展示龙门山以来经历了E-W以来〜5-2的缩短动作。我们展示了两种倾斜推进东部的倾斜分区模型，并建议西藏的东部挤压主要适用于防滑龙皮，龙门山敏山故障区。这些结果提高了我们对松潘 - 甘孜地区和四川盆地之间的构造关系的理解，为研究东部的地球动力反应到正在进行的印度碰撞的研究提供了额外的限制。 </ 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-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23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 Zhigang&option=202" target="_blank" rel="nofollow">Li Zhigang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Peizhen&option=202" target="_blank" rel="nofollow">Zhang Peizhen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Wenjun&option=202" target="_blank" rel="nofollow">Zheng Wenjun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jia Dong&option=202" target="_blank" rel="nofollow">Jia Dong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hubbard Judith&option=202" target="_blank" rel="nofollow">Hubbard Judith;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Almeida Rafael&option=202" target="_blank" rel="nofollow">Almeida Rafael;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sun Chuang&option=202" target="_blank" rel="nofollow">Sun Chuang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shi Xuhua&option=202" target="_blank" rel="nofollow">Shi Xuhua;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Tao&option=202" target="_blank" rel="nofollow">Li Tao;</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>Guangdong Provincial Key Lab of Geodynamics and Geohazards School of Earth Sciences and EngineeringSun Yat‐sen UniversityGuangzhou China;</p> <p>Guangdong Provincial Key Lab of Geodynamics and Geohazards School of Earth Sciences and EngineeringSun Yat‐sen UniversityGuangzhou China;</p> <p>Guangdong Provincial Key Lab of Geodynamics and Geohazards School of Earth Sciences and EngineeringSun Yat‐sen UniversityGuangzhou China;</p> <p>School of Earth Sciences and EngineeringNanjing UniversityNanjing China;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Guangdong Provincial Key Lab of Geodynamics and Geohazards School of Earth Sciences and EngineeringSun Yat‐sen UniversityGuangzhou China;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Guangdong Provincial Key Lab of Geodynamics and Geohazards School of Earth Sciences and EngineeringSun Yat‐sen UniversityGuangzhou 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=eastern Tibet&option=203" rel="nofollow">eastern Tibet;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Longmen Shan&option=203" rel="nofollow">Longmen Shan;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wenchuan earthquake&option=203" rel="nofollow">Wenchuan earthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oblique thrusting&option=203" rel="nofollow">oblique thrusting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=strain partitioning&option=203" rel="nofollow">strain partitioning;</a> </p> <div class="translation"> 机译：西藏东部;龙门山;汶川地震;斜推;应变分区; 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