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首页> 外文期刊>Geochemistry, geophysics, geosystems >Source‐To‐Sink Links Between East Asia and Taiwan From Detrital Zircon Geochronology of the Oligocene Huagang Formation in the East China Sea Shelf Basin
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Source‐To‐Sink Links Between East Asia and Taiwan From Detrital Zircon Geochronology of the Oligocene Huagang Formation in the East China Sea Shelf Basin

机译：东亚和台湾在德国石昌地球城地球厂中东亚海岸盆地脱尔康地球化的源区

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Abstract >Researchers have long suspected a source‐to‐sink link between the Yangtze Block (and/or North China Block) and Eocene‐Miocene passive margin strata in Taiwan, and various models have been proposed to explain similarities in provenance and the presence of Archean grains. The East China Sea Shelf Basin, whose evolution has been neglected in most models, resides between potential mainland China source regions and the sediment sink in Taiwan, and occupies the corridor through which sediment would have been transported. Here we present 378 new concordant detrital zircon U–Pb ages from the Oligocene Huagang formation in the Xihu Sag, eastern East China Sea Shelf Basin. We also present a compilation of published detrital zircon data from major rivers across mainland China to evaluate potential sediment source regions. Detrital zircons in the Huagang formation range in age from 33?±?0.4 to 2842?±?43?Ma, with major clusters at 100–300 and 1,600–2,200?Ma and small early‐middle Paleozoic, Neoproterozoic, and Paleoproterozoic to Archean peaks. Visual and statistical comparison of age distributions suggest close relationships between the Min River and Eocene–Oligocene samples from western Taiwan and between the Oligocene Huagang formation and Miocene strata in western Taiwan. Combined with the tectonic and depositional evolution of the region, these observations suggest that Eocene–Oligocene sediments in Taiwan were mainly sourced from the Min River or similar drainage in the Cathaysia Block. However, the similarities between the Huagang formation and Miocene strata are best explained by reworking of the Oligocene sediment in the Xihu Sag and transportation to western Taiwain during Miocene tectonic inversion of the East China Sea Shelf Basin. </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> >研究人员长期涉嫌长江（和/或华北地区）和台湾的何种世代被动保证金地层之间的源区线，并提出了各种模型来解释出现的相似之处和存在Archean谷物。东海货架盆地，其演进在大多数模型中被忽视，居住在潜在的大陆源地区和台湾的沉积物汇之间，并占据了沉积物的走廊。在这里，我们从东海市东部海岸盆地西湖凹陷中番茄华昌组中展示了378岁的新协调纠纷锆石U-PB。我们还撰写了来自中国大陆主要河流的发布邪恶锆石数据，以评估潜在的沉积源地区。在华昌地层中的滴乳锆石从33岁的年龄从33？±0.4到2842？±43？ma，主要簇在100-300和1,600-2,200？ma和小早期古生代，新古代古代，古普罗科奇山峰。年龄分布的视觉和统计比较表明了台湾西班湾闽河和何奥替烯样品之间的密切关系，以及台湾西部的少妇华昌地层与中肾上腺层。这些观察结果结合了该地区的构造和沉积演化，表明台湾的奥茂寡茂沉积物主要来自Min River或Jouadyia Block中的类似排水。然而，通过在东海地铁盆地的中新世构造反演期间，通过在西湖凹陷和交通到西部的西部的寡世族沉积物的重新加工来解释华昌地层和中肾上腺层之间的相似性。</ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第10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=Wang Wei&option=202" target="_blank" rel="nofollow">Wang Wei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bidgoli Tandis&option=202" target="_blank" rel="nofollow">Bidgoli Tandis;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Xianghua&option=202" target="_blank" rel="nofollow">Yang Xianghua;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ye Jiaren&option=202" target="_blank" rel="nofollow">Ye Jiaren;</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>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of GeosciencesWuhan China;</p> <p>Kansas Geological SurveyUniversity of KansasLawrence KS USA;</p> <p>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of GeosciencesWuhan China;</p> <p>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of GeosciencesWuhan 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=U–Pb&option=203" rel="nofollow">U–Pb;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yangtze&option=203" rel="nofollow">Yangtze;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=western foothills&option=203" rel="nofollow">western foothills;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hsuehshan range&option=203" rel="nofollow">Hsuehshan range;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=multidimensional scaling&option=203" rel="nofollow">multidimensional scaling;</a> </p> <div class="translation"> 机译：U-PB;长江;西山麓;Hsuehshan系列;多维缩放; </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/0704023360555.html">Source‐To‐Sink Links Between East Asia and Taiwan From Detrital Zircon Geochronology of the Oligocene Huagang Formation in the East China Sea Shelf Basin</a> 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张连昌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张连昌</a> <span> <a href="/journal-cn-57400/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿物岩石地球化学通报 </a> </span> <span> . 2007</span><span>,第z1期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_sedimentary-facies-palaeogeography_thesis/0201293597696.html">巴颜喀拉三叠纪沉积盆地岩石地球化学特征与物源区构造背景的探讨——以阿坝-若尔盖、小金-马尔康及雅江盆地为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杜德勋&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 杜德勋</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=罗建宁&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,罗建宁</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈明&option=202" target="_blank" rel="nofollow" class="tuijian_auth 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Yang Xiaoqiang</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨小强&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨小强</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Jie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Yang Jie</a> <span> <a href="/conference-cn-14627/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地球物理学会第二十五届年会 </a> <span> <span> . 2009</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020311743222.html">东亚热带地区～9000 cal.yr以来地球磁场长期变化与气候演化——来自海南岛双池岭玛珥湖的记录</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=阳杰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 阳杰</a> <span> . 2009</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130413138632.html">Method and device for transferring data and information to allow the wireless link can be estimated between the sources using a single carrier orthogonal frequency-division multiplexing and at least one receiver, and, single-carrier orthogonal frequency division multiplexing method and device for estimating a radio link between the source and the receiver using the method</a> <b>[P]</b> . <span> 外国专利： <!-- 日本专利： --> JP5986355B2 </span> <span> . 2016-09-06</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：可以使用单载波正交频分复用和至少一个接收机在源之间估计用于传输数据和信息以允许无线链路的方法和设备，以及用于估计无线电的单载波正交频分复用方法和设备。使用该方法在源和接收器之间建立链接 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130432320256.html">DECISION REGARDING THE ASSIGNMENT AND ALLOCATION OF RESOURCES FOR AT LEAST ONE DATA FLOW AND AT LEAST ONE USEABLE 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