Using Detrital Zircon Geochronology to Constrain Paleogene Provenance and Its Relationship to Rifting in the Zhu 1 Depression, Pearl River Mouth Basin, South China Sea

Wang Wei; Ye Jiaren; Bidgoli Tandis; Yang Xianghua; Shi Hesheng; Shu Yu

摘要

Abstract >Paleogene syn‐rift successions in the South China Sea are poorly understood and systematic provenance analysis, which could provide clues to their history, is lacking. Here we report 409 new concordant U‐Pb ages from detrital zircons separated from the Paleogene Wenchang, Enping, and Zhuhai formations in the Zhu 1 depression, Pearl River Mouth Basin. The new data, combined with the published age data from the region, document changes in the provenance of syn‐rift successions. Detrital zircons from the Eocene Wenchang Formation are unimodal, with Jurassic‐Cretaceous (180–80 Ma) ages making up 80% of grains. The ages are consistent with the geochronology of intrabasinal highs, dominated by igneous rocks emplaced during the Yanshanian orogeny, and suggest local provenance. By contrast, detrital zircons from the upper Eocene to lower Oligocene Enping Formation form three well‐recognized age‐clusters, with peaks at 150, 254, and 438 Ma that match documented tectonomagmatism in South China Block (SCB). Combined with increasing numbers of Precambrian zircons, the data suggest increasing influence of regional provenance of the SCB. Similar age peaks are also recognized from the limited number of zircons analyzed from the upper Oligocene Zhuhai Formation and comparability with modern shelf and river sediment indicates the unit was mainly sourced from the SCB and likely transported by a paleo‐Pearl River. We infer that the change in provenance, from local uplifts within the Zhu 1 to the SCB, is related to distinct phases of PRMB rift development; however, later changes are best explained by SCB drainage evolution. </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> <P>古代南海的古速溶性继承率较差，理解和系统的出处分析，可以为其历史提供线索，缺乏。在这里，我们从诸如古代文昌，恩平和珠海地层中分开的碎屑锆石来报告409年的新协调y-Pb年龄，珠宝抑郁症，珠江口盆地。新数据与来自该地区的公布年龄数据相结合，文档在Syn-Rift演替的出处中的变化。来自鄂科文昌地层的拆伤锆石是单峰的，侏罗纪 - 白垩纪（180-80 mA）弥补＆ 80％的谷物。年龄符合内部高位的地理学，由燕山山脉越来置的火成岩，并建议当地的出处。相比之下，来自上何世欧世的滴乳氧化锆给下寡核苷恩平形成，形成了三种公认的年龄簇，达到了150,254和438 mA的峰，与华南地区（SCB）匹配了记录的Tectononomatism。结合越来越多的前锋锆石，数据表明了SCB区域出处的影响。类似的年龄峰也从珠海上部珠海的上寡核苷珠海形成和现代货架和河流沉积物的可比性中识别出有限数量的锌，表明该单位主要来自SCB，可能由古珠江河流运输。我们推断从朱1到SCB内的当地隆起的出处的变化与PRMB裂缝发展的不同阶段有关;但是，SCB排水进化最好解释后来的变化。</ 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>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共24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=Ye Jiaren&option=202" target="_blank" rel="nofollow">Ye Jiaren;</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=Shi Hesheng&option=202" target="_blank" rel="nofollow">Shi Hesheng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shu Yu&option=202" target="_blank" rel="nofollow">Shu Yu;</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>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of GeosciencesWuhan China;</p> <p>Kansas Geological SurveyUniversity of KansasLawrence Kansas USA;</p> <p>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of GeosciencesWuhan China;</p> <p>Shenzhen Branch of China National Offshore Oil Corporation Ltd.Guangzhou China;</p> <p>Shenzhen Branch of China National Offshore Oil Corporation Ltd.Guangzhou 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=source‐to‐sink&option=203" rel="nofollow">source‐to‐sink;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South China Block&option=203" rel="nofollow">South China Block;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wenchang Formation&option=203" rel="nofollow">Wenchang Formation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yanshanian&option=203" rel="nofollow">Yanshanian;</a> </p> <div class="translation"> 机译：U-PB;源到汇;华南区块;文昌地层;燕山; </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> </ul> 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