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Crustal Radial Anisotropy and Linkage to Geodynamic Processes: A Study Based on Seismic Ambient Noise in Southern Madagascar

机译：地壳径向各向异性和地球动力学过程的联系：基于马达加斯加南部地震环境噪声的研究

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Abstract > We determined radial anisotropy in the crust of southern Madagascar from the differences between the speeds of vertically and horizontally polarized shear waves ( <fi>V</fi> <sub>SV</sub> and <fi>V</fi> <sub>SH</sub> ), which we derived from Rayleigh and Love wave dispersion determined from seismic ambient noise correlations. The amalgamated Precambrian units in the east and the Phanerozoic Morondava basin in the west of southern Madagascar were shaped by different geodynamic processes. The crystalline basement was strongly deformed and metamorphosed to varying degrees during the assembly of Gondwana in the Pan‐African Orogeny, whereas the Morondava basin was completed with the separation of Africa and Madagascar. The different developments are reflected in first‐order differences in the radial anisotropy patterns. In the Precambrian domains, positive anisotropy ( <fi>V</fi> <sub>SV</sub> < <fi>V</fi> <sub>SH</sub> ) is found in the upper and lower crust, with a layer of negative anisotropy ( <fi>V</fi> <sub>SV</sub> > <fi>V</fi> <sub>SH</sub> ) sandwiched in between. The upper crustal anisotropy may reflect shallowly dipping layering within the Archean and adjacent imbricated nappe stacks, whereas the lower crustal anisotropy likely represents fossilized crustal flow during the postorogenic or synorogenic collapse of the Pan‐African Orogen. The negative anisotropy layer may have preserved vertically oriented large shear zones of late Pan‐African age. Within the Morondava basin, negative anisotropy in the uppermost ～5?km could have been generated by steep normal faults, jointing, and magmatic dike intrusions. The deeper sediments and underlying crustal basement are characteri </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”XML：ID =“JGRB52854-Abs-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> >我们确定了外壳中的径向各向异性Madagascar南部来自垂直和水平偏振剪切波的速度之间的差异（<fi> V </ fi> <sub> sv </ sub>和<fi> v </ fi> <sh </ sub>），我们从瑞利和爱波色散中得出的，从地震环境噪声相关性决定。在马达加斯加南部西部的东部和Phanerozoice Morondava盆地的合并前锋单位被不同的地球动力学过程塑造。在泛非洋地构的Gondwana组装过程中，结晶地下室强烈地变形并变成了不同程度的变色，而Morondava盆地在非洲和马达加斯加的分离完成。不同的发展反映在径向各向异性模式中的一阶差异。在前方地壳中发现了阳性各向异性（<fi> v </ fi> sv </ sub> <fi> v </ fi> <sh </ sub>），具有一层阴性各向异性（<fi> v </ fi> <sub> sv </ sub <fi> v </ fi> <sum> sh </ sub>）。上部地壳各向异性可能反映了阿奇和相邻的覆层堆叠内的浅层浸渍分层，而下的地壳各向异性可能代表泛非造成泛非orgen的后造成或纵向塌陷期间的化散液面流动。阴性各向异性层可能已经保存过垂直定向的大型泛非洲时代的大剪切区。在Morondava盆地内，最高〜5 km最高的各向异性可以通过陡峭的正常断层，连接和岩浆堤防入侵来产生。更深层次的沉积物和底层地下室是特征 </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17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=Dreiling Jennifer&option=202" target="_blank" rel="nofollow">Dreiling Jennifer;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tilmann Frederik&option=202" target="_blank" rel="nofollow">Tilmann Frederik;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yuan Xiaohui&option=202" target="_blank" rel="nofollow">Yuan Xiaohui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Giese J?rg&option=202" target="_blank" rel="nofollow">Giese J?rg;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rindraharisaona Elisa J.&option=202" target="_blank" rel="nofollow">Rindraharisaona Elisa J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rümpker Georg&option=202" target="_blank" rel="nofollow">Rümpker Georg;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wysession Michael E.&option=202" target="_blank" rel="nofollow">Wysession Michael E.;</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>GFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>GFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>GFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Freie Universit?t BerlinBerlin Germany;</p> <p>GFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Institute of GeosciencesGoethe‐Universit?t FrankfurtFrankfurt am Main Germany;</p> <p>Department of Earth and Planetary SciencesWashington UniversitySaint Louis USA;</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;"> </p> </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/0704025591791.html">Crustal Radial Anisotropy and Linkage to Geodynamic Processes: A Study Based on Seismic Ambient Noise in Southern Madagascar</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dreiling Jennifer&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dreiling Jennifer,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tilmann Frederik&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tilmann Frederik,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yuan Xiaohui&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yuan Xiaohui,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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