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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Paleomagnetic Study on the Permian Rocks of the Indochina Block and Its Implications for Paleogeographic Configuration and Northward Drifting of Cathaysialand in the Paleo‐Tethys
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Paleomagnetic Study on the Permian Rocks of the Indochina Block and Its Implications for Paleogeographic Configuration and Northward Drifting of Cathaysialand in the Paleo‐Tethys

机译：古地区古代岩石岩石岩石古代岩石的古磁性研究及古地理构造与北方漂移的古代特质

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Abstract > The drift of Gondwana‐derived blocks across the Tethys has remained unclear specifically because one of the largest components, Indochina, has remained unconstrained by paleomagnetism during the late Paleozoic, the interval comprising the first half of its journey towards the Eurasian landmass. Hence, we report a paleomagnetic study of Early‐Middle Permian limestones from central Thailand yielding a high‐quality data set for the Indochina Block with probable primary origin. The magnetization yields a paleomagnetic pole at 34.1°N, 331.7°E ( K ?=?45.4, A <sub>95</sub> ?=?5.7°) corresponding to a paleolatitude of 21.2?±?5.7°S at the center of the study area (15°N, 101°E) and supporting a tropical restoration for late Paleozoic Indochina. A total of ~5,000?km northward transition from a proximity to Gondwana in the Early‐Middle Permian (ca. 280?Ma) to the southern margin of Eurasia by the Late Triassic (Norian, ca. 220?Ma) is identified and yields an average northward latitudinal drift rate of ~4.5?cm/year. A concurrent northward drifting history during the Permian is suggested for the Indochina, North Qiangtang, and South China blocks, and thus, the widely used model of Permian Cathaysialand is quantitively supported when combined with their paleobiogeographic affinities. </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”> <title类型=“main”>抽象</ title> > Thethys对Gondwana派生块的漂移仍然不清楚，因为最大的一个在古生代晚期的古代古代古代的古代古代，组件吲哚china一直不受约束，该间隔包括其前半部分朝向欧亚陆地的旅程。因此，我们举行了泰国中部早期二叠系石灰岩的古磁性研究，从而为吲哚ININA阻滞具有可能的主要原因的高质量数据。磁化强度在34.1°N，331.7°E（ k </ i>α=Δ45.4，<sub> 95）对应于21.2的古孔（ k </ i>α=Δ45.4）时产生古磁磁极。 ±5.7°S在研究区域的中心（15°N，101°E）并支持晚古生代印度吲哚靛蓝的热带恢复。从晚期二叠纪（Jorian，CA.220？MA）的欧亚欧亚南部的欧亚南部的欧亚南部的南部边缘，总共〜5,000？Km向北过渡。确定并收益平均北部纬度漂移率〜4.5？cm /年。在二叠纪，北羌塘和华南区块建议了同时的北方漂移历史，因此，当与古食电性亲和力结合时，定量支持广泛使用的二叠纪菊花模型。 </ 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6期</span><b style="margin: 0 2px;">|</b><span>共16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=Yan Yonggang&option=202" target="_blank" rel="nofollow">Yan Yonggang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Baochun&option=202" target="_blank" rel="nofollow">Huang Baochun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Donghai&option=202" target="_blank" rel="nofollow">Zhang Donghai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Charusiri Punya&option=202" target="_blank" rel="nofollow">Charusiri Punya;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Veeravinantanakul Apivut&option=202" target="_blank" rel="nofollow">Veeravinantanakul Apivut;</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>Key Laboratory of Orogenic Belt and Crust Evolution Ministry of Education School of Earth and Space SciencesPeking UniversityBeijing China;</p> <p>Key Laboratory of Orogenic Belt and Crust Evolution Ministry of Education School of Earth and Space SciencesPeking UniversityBeijing China;</p> <p>Earthquake and Tectonic Geology Research Unit (EATGRU) c/o Department of Geology Faculty of ScienceChulalongkorn UniversityBangkok Thailand;</p> <p>Earthquake and Tectonic Geology Research Unit (EATGRU) c/o Department of Geology Faculty of ScienceChulalongkorn UniversityBangkok Thailand;</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=paleomagnetism&option=203" rel="nofollow">paleomagnetism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P ermian&option=203" rel="nofollow">P ermian;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=I ndochina&option=203" rel="nofollow">I ndochina;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=C athaysialand&option=203" rel="nofollow">C athaysialand;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T ethys&option=203" rel="nofollow">T ethys;</a> </p> <div class="translation"> 机译：颅骨磁性;P ermanian;我是手机;c acysialand;t ethys; </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> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025592787.html">Paleomagnetic Study on the Permian Rocks of the Indochina Block and Its Implications for Paleogeographic Configuration and Northward Drifting of Cathaysialand in the Paleo‐Tethys</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Yonggang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yan Yonggang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Baochun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Huang Baochun,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Donghai&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Donghai,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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