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Tectonic Topography Changes in Cenozoic East Asia: A Landscape Erosion‐Sediment Archive in the South China Sea

机译：新生代东亚的构造地形变化：南海横向侵蚀沉积物档案

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Abstract > The mode and tempo of Cenozoic fluvial input into the South China Sea by Asian rivers were strongly controlled by tectonically induced topographic changes and landscape development that resulted in repeated river captures and reversals. New Nd isotope and U‐Pb detrital zircon data from clastic sedimentary sequences in the northern South China Sea display secular variations reflecting significant changes in the compositions of fluvial sediment as well as changes in source rocks. The oldest, Eocene‐Oligocene (before ～25 Ma) clastic rocks of the South China Sea contain sediments with ? <sub>Nd</sub> values of ?5 to ?7.5 and detrital zircons of Cretaceous, Jurassic, and Permo‐Triassic, all derived from southern Cathaysia. The Oligocene‐Middle Miocene (～25–11 Ma) sediments in the South China Sea strata display ? <sub>Nd</sub> values of ?12 to ?14 and Archean, Proterozoic, and Paleozoic detrital zircons, suggesting northern Cathaysia and/or the Yangtze Blocks as their provenance. The headward expansion of the Pearl River and reversal of the Middle Yangtze River correlates with the opening of the South China Sea and growth of the eastern Tibetan Plateau at ～25 Ma. Further uplift of the eastern Tibetan Plateau and the Wuyi‐Nanling Mountains in SE China around 11 Ma reshaped the landscape and caused another phase of erosion—pattern adjustment and drainage—divide migration in East Asia, leading to the establishment of the modern fluvial systems of the Pearl, Minjiang, and Lower Yangtze Rivers. </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”> <标题类型=“main”>抽象</ title> > 亚洲河流南海的新生代流入南海进入的模式和节奏受到强调诱导的地形变化和景观发展，导致反复河流捕获和逆转。新的ND同位素和南海北部泥炭沉积序列的U-PB拆卸锆石数据显示了河流沉积物组合物的近似变化，以及源岩的变化。最古老，南海的玉米龙（在〜25 mA之前）南海的碎片岩石含有沉积物？</ b> <sub> nd </ sub> ？5到？7.5和邪恶的白垩纪，侏罗纪和渗透锆石的价值观，所有这些都来自于加州南部的南部。南海地层展示中寡烯 - 中生（〜25-11 mA）沉积物？</ b> <sub> nd </ sub> ？12到？14和Archean，Norlozeoic和古生代碎屑锆石的价值观，暗示了北部的Jourthern和/或长江作为他们的出处。珠江珠江的前向膨胀与中长江的逆转与南海开放和东藏高原的增长在〜25 mA的开放相关。藏高原的进一步隆起和武夷南陵山脉在SE中国左右11 mA重塑了景观，并引起了东亚侵蚀模式调整和排水划分的另一种阶段，导致建立现代河流系统珍珠，岷江和较低的长江河。 </ 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6期</span><b style="margin: 0 2px;">|</b><span>共20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 Yi&option=202" target="_blank" rel="nofollow">Yan Yi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Deng&option=202" target="_blank" rel="nofollow">Yao Deng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tian Zhi‐Xian&option=202" target="_blank" rel="nofollow">Tian Zhi‐Xian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Chi‐Yue&option=202" target="_blank" rel="nofollow">Huang Chi‐Yue;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dilek Yildirim&option=202" target="_blank" rel="nofollow">Dilek Yildirim;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Clift Peter D.&option=202" target="_blank" rel="nofollow">Clift Peter D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Zi‐An&option=202" target="_blank" rel="nofollow">Li Zi‐An;</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 Ocean and Marginal Sea GeologyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>Key Laboratory of Ocean and Marginal Sea GeologyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>Key Laboratory of Ocean and Marginal Sea GeologyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>Key Laboratory of Ocean and Marginal Sea GeologyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>Department of Geology &</p> <p>Environmental Earth ScienceMiami UniversityOH USA;</p> <p>Department of Geology and GeophysicsLouisiana State UniversityBaton Rouge LA USA;</p> <p>School of Marine SciencesSun 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=South China Sea&option=203" rel="nofollow">South China Sea;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nd isotopes of fluvial sediments&option=203" rel="nofollow">Nd isotopes of fluvial sediments;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=East Asian Rivers&option=203" rel="nofollow">East Asian Rivers;</a> <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=Pearl River&option=203" rel="nofollow">Pearl River;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yangtze River&option=203" rel="nofollow">Yangtze River;</a> </p> <div class="translation"> 机译：南海;河流沉积物的同位素;东亚河流;西藏;珠江;长江;长江; </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/0704023360737.html">Tectonic Topography Changes in Cenozoic East Asia: A Landscape Erosion‐Sediment Archive in the South China Sea</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yan Yi&option=202" target="_blank" rel="nofollow" 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