首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Post‐rift Tectonic History of the Songliao Basin, NE China: Cooling Events and Post‐rift Unconformities Driven by Orogenic Pulses From Plate Boundaries

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Post‐rift Tectonic History of the Songliao Basin, NE China: Cooling Events and Post‐rift Unconformities Driven by Orogenic Pulses From Plate Boundaries

机译：松辽盆地松辽盆地的后裂变构造历史：由板边界造时脉冲驱动的冷却事件和裂缝后无关

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Abstract >The classic lithosphere‐stretching model predicts that the post‐rift evolution of extensional basin should be exclusively controlled by decaying thermal subsidence. However, the stratigraphy of the Songliao Basin in northeastern China shows that the post‐rift evolution was punctuated by multiple episodes of uplift and exhumation events, commonly attributed to the response to regional tectonic events, including the far‐field compression from plate margins. Three prominent tectonostratigraphic post‐rift unconformities are recognized in the Late Cretaceous strata of the basin: T11, T03, and T02. The subsequent Cenozoic history is less constrained due to the incomplete record of younger deposits. In this paper, we utilize detrital apatite fission track (AFT) thermochronology to unravel the enigmatic timing and origin of post‐rift unconformities. Relating the AFT results to the unconformities and other geological data, we conclude that in the post‐rift stage, the basin experienced a multiepisodic tectonic evolution with four distinct cooling and exhumation events. The thermal history and age pattern document the timing of the unconformities in the Cretaceous succession: the T11 unconformity at ~88–86?Ma, the T03 unconformity at ~79–75?Ma, and the T02 unconformity at ~65–50?Ma. A previously unrecognized Oligocene unconformity is also defined by a ~32–24?Ma cooling event. Tectonically, all the cooling episodes were regional, controlled by plate boundary stresses. We propose that Pacific dynamics influenced the wider part of eastern Asia during the Late Cretaceous until Cenozoic, whereas the far‐field effects of the Neo‐Tethys subduction and collision processes became another tectonic driver in the later Cenozoic. </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 =“Ru”> <标题类型=“main”>抽象</ title> >经典的岩石圈拉伸模型预测扩大盆地的后裂缝演变应该是专门的通过腐烂的热沉降控制。然而，中国东北部的松辽盆地的地层表明，裂口后进化被隆起和挖掘事件的多集，通常归因于对区域构造事件的响应，包括从板条边缘的远场压缩。在盆地的晚期白垩纪地层中识别出三个突出的构造数据术后不整合：T11，T03和T02。由于年轻存款的不完整记录，随后的新生代历史不受限制。在本文中，我们利用滴乳透散轨（AFT）热量来解开裂变的不整合的神秘时序和起源。向后结果与其他地质数据联系起来，我们得出结论，在裂口后阶段，盆地经历了具有四种不同的冷却和挖掘事件的多透视构造演变。热历史和年龄模式文件在白垩纪连续中的不一致系数中：T11不整合在〜88-86？ma，T03在〜79-75〜79-75〜65-50的T02不整合。以前未被识别的寡核苷酸不整合也由〜32-24？MA冷却事件定义。构造上，所有冷却发作都是区域，由板边界应力控制。我们提出太平洋动态影响了东亚的更广泛的白垩纪宽德一部分，直到新生代，而Neo-Threthys俯冲和碰撞过程的远场效果成为后来新生代的另一个构造司机。</ 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3期</span><b style="margin: 0 2px;">|</b><span>共33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=Song Ying&option=202" target="_blank" rel="nofollow">Song Ying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stepashko Andrei&option=202" target="_blank" rel="nofollow">Stepashko Andrei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Keyu&option=202" target="_blank" rel="nofollow">Liu Keyu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=He Qingkun&option=202" target="_blank" rel="nofollow">He Qingkun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shen Chuanbo&option=202" target="_blank" rel="nofollow">Shen Chuanbo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shi Bingjie&option=202" target="_blank" rel="nofollow">Shi Bingjie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ren Jianye&option=202" target="_blank" rel="nofollow">Ren Jianye;</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>Department of GeologyChina University of Petroleum (East China)Qingdao China;</p> <p>Kosygin Institute of Tectonics and Geophysics Far Eastern BranchRussian Academy of SciencesKhabarovsk Russia;</p> <p>Department of GeologyChina University of Petroleum (East China)Qingdao China;</p> <p>School of Materials Science and EngineeringShandong University of Science and TechnologyQingdao China;</p> <p>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of Geosciences (Wuhan)Wuhan China;</p> <p>Department of Earth and Environmental SciencesUniversity of WaterlooWaterloo Ontario Canada;</p> <p>Key Laboratory of Tectonics and Petroleum Resources Ministry of EducationChina University of Geosciences (Wuhan)Wuhan 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=postrift&option=203" rel="nofollow">postrift;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Songliao Basin&option=203" rel="nofollow">Songliao Basin;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=detrital apatite fission track&option=203" rel="nofollow">detrital apatite fission track;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=unconformity&option=203" rel="nofollow">unconformity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pacific plate&option=203" rel="nofollow">Pacific plate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Neo‐Tethys&option=203" rel="nofollow">Neo‐Tethys;</a> </p> <div class="translation"> 机译：Postrift;松辽盆地;滴乳磷灰石裂变轨道;不整合;太平洋板块;Neo-Thethys; 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tuijian_authcolor">,王铁军</a> <span> <a href="/journal-cn-4885/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质学报 </a> </span> <span> . 2020</span><span>,第010期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_petroleum-geology-experiment_thesis/0201218282896.html">一个大型弧后裂谷盆地的沉积充填模式 --以松辽盆地为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈建文&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈建文</a> <span> <a href="/journal-cn-7900/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 石油实验地质 </a> </span> <span> . 2000</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_earth-science-journal-china-university-geosciences_thesis/0201293064106.html">伸展构造盆地的平衡剖面及其构造意义——以松辽盆地南部为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=颜丹平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 颜丹平</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=田崇鲁&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,田崇鲁</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孟令波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,孟令波</a> <span> <a href="/journal-cn-50713/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地球科学：中国地质大学学报 </a> </span> <span> . 2003</span><span>,第3期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-35319_thesis/020221275460.html">一个大型弧后裂谷盆地的沉积充填模式——以松辽盆地为例</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈建文&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈建文</a> <span> <a href="/conference-cn-35319/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第四届全国沉积学及岩相古地理学术研讨会 </a> <span> <span> . 1995</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314349531.html">松辽盆地徐家围子断陷构造特征研究：基于构造物理模拟分析</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=龙伟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 龙伟</a> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130438907272.html">Framework for e.g. wash basin, has lower frame with two vertical posts integrated to horizontal bearing plates for fixing on horizontal plane, and reinforcement gusset placed behind each post and also fixed on corresponding plates</a> <b>[P]</b> . <span> 外国专利：  FR2868097A1 </span> <span> . 2005-09-30</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：例如的框架洗脸盆，下部框架，带有两个垂直立柱，集成到水平支撑板上以固定在水平面上，加固角撑板放置在每个立柱的后面并固定在相应的板上 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130436606933.html">Joint for front walls or corner posts of folding flat rack container, has opening cut to interior surface adjacent to boundary wall of inner joint plate to lodge corner of container into corner fitting of baseplate</a> <b>[P]</b> . <span> 外国专利：  DE202005017844U1 </span> <span> . 2006-02-23</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：折叠式扁平货架容器的前壁或角柱的接头，在与内接头板的边界壁相邻的内表面开有切口，以将容器的角部放入底板的角部中 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130440041221.html">Fencing system uses anchoring elements formed with base plate and at least one projection of suitable shape fastened under base plate, so as to be able to be pushed or driven into ground to fix posts supporting fence</a> <b>[P]</b> . <span> 外国专利：  NL1028562C1 </span> <span> . 2005-09-20</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：围栏系统使用锚固元件，该锚固元件由底板和至少一个合适形状的突起固定在底板下方，以便能够推入或打入地面以固定支撑围栏的柱子 </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('0704025591977','4',7,2,1,'',this,24)" class="delivery" 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