3‐D Crustal Shear‐Wave Velocity Structure of the Taiwan Strait and Fujian, SE China, Revealed by Ambient Noise Tomography

Zhang Yayun; Yao Huajian; Yang Hsin‐Ying; Cai Hui‐Teng; Fang Hongjian; Xu Jiajun; Jin Xing; Kuo‐Chen Hao; Liang Wen‐Tzong; Chen Kai‐Xun

摘要

Abstract >The Taiwan Strait, along with the southeastern continental margin of the Eurasian plate, Fujian in SE China, is not far from the convergent boundary between the Eurasian plate and the Philippine Sea plate. Although this region is considered tectonically relatively inactive, many small earthquakes still occur, and normal faults are well developed in the strait. To better understand the geological processes in this region, we use 2?years of ambient noise data from more than 100 stations in Fujian and Taiwan to obtain a 3‐D crustal shear‐wave velocity model using a direct surface‐wave inversion method. Our results show that the low‐velocity zone beneath the Zhenghe‐Dapu suture zone plays an important role in the tectonic evolution of the Fujian area. The relatively high velocity in the eastern part of the suture zone and low velocity in the west correspond to the Mesozoic magmatic zone and the Wuyi‐Yunkai orogenic belt in Fujian, respectively. The coastline of Fujian presents a high‐velocity anomaly in the upper crust, which is related to the Mesozoic Pingtan‐Dongshan metamorphic belt. The long strip‐like high‐velocity zone through the rift basins in the strait is interpreted as igneous rocks due to extension of the lithosphere in the Cenozoic. Two‐stage extension with different extensive centers in the strait may be the reason for the high‐ and low‐velocity anomalies in the middle to lower crust and uppermost mantle of the strait. </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 type =“main”>抽象</ title> >台湾海峡，以及欧亚板块的东南大陆边缘，福建在SE中国，离欧亚板块和菲律宾海底之间的会聚边界不远。虽然该地区被认为是根本相对不活跃的，但仍然发生了许多小地震，并且在海峡中发育了正常的故障。为了更好地了解该地区的地质过程，我们使用来自福建和台湾100多站的2年的环境噪声数据，使用直接表面波反转方法获得3d地壳剪切波速度模型。我们的研究结果表明，诸暨缝合区下面的低速区在福建地区的构造演变中起着重要作用。缝合区的东部的相对高的速度和西部的低速相对应于福建省中生代岩石区和武夷yungai造山带。福建海岸线在上层地壳中呈现出高速异常，这与中生代平潭 - 东山变形带有关。由于新生代岩石圈的延伸，通过海峡中裂缝盆地的长条状高速区通过裂缝盆地被解释为火岩。海峡中不同广泛中心的两阶段延伸可能是中间地壳和海峡最上面的地壳和最上面的地幔中的高速和低速异常的原因。</ 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9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=Zhang Yayun&option=202" target="_blank" rel="nofollow">Zhang Yayun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Huajian&option=202" target="_blank" rel="nofollow">Yao Huajian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Hsin‐Ying&option=202" target="_blank" rel="nofollow">Yang Hsin‐Ying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cai Hui‐Teng&option=202" target="_blank" rel="nofollow">Cai Hui‐Teng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fang Hongjian&option=202" target="_blank" rel="nofollow">Fang Hongjian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Jiajun&option=202" target="_blank" rel="nofollow">Xu Jiajun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jin Xing&option=202" target="_blank" rel="nofollow">Jin Xing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kuo‐Chen Hao&option=202" target="_blank" rel="nofollow">Kuo‐Chen Hao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liang Wen‐Tzong&option=202" target="_blank" rel="nofollow">Liang Wen‐Tzong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Kai‐Xun&option=202" target="_blank" rel="nofollow">Chen Kai‐Xun;</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>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Earthquake Administration of Fujian ProvinceFuzhou China;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Earthquake Administration of Fujian ProvinceFuzhou China;</p> <p>Department of Earth SciencesNational Central UniversityTaoyuan Taiwan;</p> <p>Academia SinicaInstitute of Earth SciencesTaipei Taiwan;</p> <p>Department of Earth SciencesNational Central UniversityTaoyuan Taiwan;</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=ambient noise&option=203" rel="nofollow">ambient noise;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal structure&option=203" rel="nofollow">crustal structure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=direct inversion&option=203" rel="nofollow">direct inversion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=two‐stage extension&option=203" rel="nofollow">two‐stage extension;</a> </p> <div class="translation"> 机译：环境噪声;地壳结构;直接反演;两级延伸; 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