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首页> 外文期刊>Geochemistry, geophysics, geosystems >Paleomagnetic Constraints on the Middle Miocene‐Early Pliocene Stratigraphy in the Xining Basin, NE Tibetan Plateau, and the Geologic Implications
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Paleomagnetic Constraints on the Middle Miocene‐Early Pliocene Stratigraphy in the Xining Basin, NE Tibetan Plateau, and the Geologic Implications

机译：西宁盆地，网藏高原高原中间内科 - 早期全茂地层的古磁性约束及地质意义

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摘要

Abstract >The Xining Basin lies in the transitional zone between the arid Asian interior and the East Asian monsoon region. The continuous Cenozoic sediments in the basin provide a unique archive recording the uplift of the Tibetan Plateau and its environmental effects on central Asian aridification and Asian monsoon evolution. However, sediments deposited since the middle Middle Miocene have not been precisely dated, hindering our ability to address these issues. Here we dated a 336 m‐thick section containing many Late Miocene fossil mammals from the eastern basin. High‐resolution paleomagnetism revealed 16 normal and 16 reversed zones that correlate well with chrons 3n to 5Ar.1r of the Geomagnetic Polarity Time Scale, constraining the section to ～12.7–4.8 Ma. The changes in lithofacies from floodplain to braided river at ～8.6 Ma and to thick alluvial fan at ～6.3 Ma with predominantly southerly paleocurrent directions occur simultaneously with an increase in the sedimentation rates, representing two periods of rapid uplift in the eastern Qilian Shan to the north. Our results provide a robust oldest age constraint (4.8 Ma) on the ancient Huang Shui and Yellow River terraces on the basin sediments and eolian deposits on the terraces. The presence of well‐developed floodplain paleosols, shallow lake marls, and many large mammals in the lower section suggests that the monsoon climate in the late Middle Miocene to Late Miocene was more humid and stronger than that at present. </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> >西宁盆地位于干旱亚洲内部和东亚季风区之间的过渡带。盆地的连续新生代沉积物提供了独特的档案，录制了藏高原的隆起及其对中亚领导和亚洲季风演化的环境影响。然而，沉积物沉积的沉积物以来尚未精确地日期，阻碍了我们解决这些问题的能力。在这里，我们用了来自东部盆地的许多晚期内烯化石哺乳动物的336米厚的部分。高分辨率古磁石揭示了16个正常和16个反向区域，其与地磁极性时间尺度的计数3N至5AR1R相关，约束该部分至约12.7-4.8 mA。来自苏洪水的岩石酸岩〜8.6 mA和厚的冲积风扇在〜6.3 mA的厚度古电流方向上同时出现了沉降率的同时发生，代表了东祁连山的快速隆起的两个时期北。我们的结果在古老的黄水和盆地沉积物上的古老黄水和黄河露台上提供了一个稳健的古老约束（＆ 4.8 ma）。在较良好的洪泛区古玉米醇，浅湖玛尔斯和大量大部分大型哺乳动物的存在表明，中间中部后期中西茂的季风气候比目前更潮湿，更强烈。</ 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=Yang Rongsheng&option=202" target="_blank" rel="nofollow">Yang Rongsheng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fang Xiaomin&option=202" target="_blank" rel="nofollow">Fang Xiaomin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meng Qingquan&option=202" target="_blank" rel="nofollow">Meng Qingquan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zan Jinbo&option=202" target="_blank" rel="nofollow">Zan Jinbo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Weilin&option=202" target="_blank" rel="nofollow">Zhang Weilin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Tao&option=202" target="_blank" rel="nofollow">Deng Tao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Yibo&option=202" target="_blank" rel="nofollow">Yang Yibo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ruan Xiaobai&option=202" target="_blank" rel="nofollow">Ruan Xiaobai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Liye&option=202" target="_blank" rel="nofollow">Yang Liye;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Bingshuai&option=202" target="_blank" rel="nofollow">Li Bingshuai;</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>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>School of Earth Sciences and Key Laboratory of Western China's Mineral Resources of Gansu ProvinceLanzhou UniversityLanzhou China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>Institute of Vertebrate Paleontology and Paleoanthropology Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing China;</p> <p>CAS Center for Excellence in Tibetan Plateau Earth Sciences and Key Laboratory of Continental Collision and Plateau UpliftInstitute of Tibetan Plateau Research Chinese Academy of SciencesBeijing 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=uppermost Cenozoic stratigraphic sequence&option=203" rel="nofollow">uppermost Cenozoic stratigraphic sequence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xining Basin&option=203" rel="nofollow">Xining Basin;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magnetostratigraphy&option=203" rel="nofollow">magnetostratigraphy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Late Miocene‐Early Pliocene&option=203" rel="nofollow">Late Miocene‐Early Pliocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=eastern Qilian Shan uplift&option=203" rel="nofollow">eastern Qilian Shan uplift;</a> </p> <div class="translation"> 机译：最上面的新生代地层序列;西宁盆地;磁子 - 早期的岩浆早期的专业;东祁连山隆起; </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"> 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<div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201293745618.html">叠合盆地成藏流体源类型、演化及控藏意义——以中国南方中、古生界海相地层为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐思煌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 徐思煌</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=袁彩萍&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,袁彩萍</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=梅廉夫&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,梅廉夫</a> <span> <a href="/journal-cn-56880/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质科技情报 </a> </span> <span> . 2007</span><span>,第2期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-geomechanics_thesis/0201253297530.html">青藏高原东北缘共和盆地第四纪磁性地层学研究</a> <b>[J]</b> <span> <a 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孟庆泉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,孟庆泉</a> <span> <a href="/conference-cn-41442/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2017年中国地球科学联合学术年会（CGU2017) </a> <span> <span> . -1</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314357975.html">青藏高原沱沱河地区中新世五道梁组磁性地层与古环境演变研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李军鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李军鹏</a> <span> . 2008</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130416441102.html">Method for exploiting sedimentary basin crossed by well for petroleum exploration, involves generating heat flow map of basin by interpolation of heat flow at base of basin for each geological time, and exploiting basin by heat flow maps</a> <b>[P]</b> . <span> 外国专利： <!-- 法国专利： --> FR2996038A1 </span> <span> . 2014-03-28</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：一种用于石油勘探的井下沉积盆地的开发方法，包括通过对每个地质时间在盆地底部的热流进行插值来生成盆地的热流图，并通过热流图来开发盆地 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130442355638.html">METHOD OF GENERATING 3-D GEOLOGIC MODELS INCORPORATING GEOLOGIC AND GEOPHYSICAL CONSTRAINTS</a> <b>[P]</b> . <span> 外国专利： <!-- --> MY116873A </span> <span> . 2004-04-30</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：结合地质和地球物理约束的3D地质模型的生成方法 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130451610559.html">Method of generating 3-D geologic models incorporating geologic and geophysical constraints</a> <b>[P]</b> . <span> 外国专利： <!-- 美国专利： --> US5838634A </span> <span> . 1998-11-17</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：结合地质和地球物理约束的3-D地质模型的生成方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360284','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div 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