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Timing of Okhotsk Sea Plate Collision With Eurasia Plate: Zircon U‐Pb Age Constraints From the Sakhalin Island, Russian Far East

机译：Okhotsk Sea Plate碰撞与欧亚邦的时序：Zircon U-PB来自Sakhalin Island，俄罗斯远东

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Abstract >The Late Mesozoic to Cenozoic evolution of Northeast Asia involves successive subduction of the Pacific oceanic crust and amalgamation of the Eurasia, North American, and Okhotsk Sea Plates. The timing of plate collision is essential for understanding the tectonic evolution of Northeast Asia. In this study, we focus on the Okhotsk Sea Plate collision with the Eurasia Plate along the Sakhalin Island, Russian Far East, which is a highly controversial problem, especially about the timing of collision. In order to determine exact timing for this collision, we report zircon U‐Pb data from both the East Sakhalin accretionary complex and postcollisional granitic plutons in the Sakhalin Island. Detrital zircon data from four metasedimentary rocks show that the Sikhote‐Alin orogenic belt is the main provenance for the East Sakhalin accretionary complex. Meanwhile, the youngest detrital zircon age constrains the maximum depositional age of East Sakhalin accretionary complex later than 49?Ma. Both Langeri and Val'za plutons are made of peraluminous S‐type granite. Four granitic samples yielded consistent ages at 36–38?Ma, indicating that both plutons were emplaced at the middle Eocene. Their generation is considered to have been derived through crustal anatexis of accretionary wedge in the lower crust shortly after tectonic thickening caused by the Okhotsk Sea Plate collision with the Eurasia Plate. Consequently, our age data constrain that the Okhotsk Sea Plate and Eurasia Plate collision occurred in the middle Eocene between 49 and 38?Ma. This age range is consistent with late Eocene uncomformity identified in the Sakhalin Island and Okhotsk Sea. </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”> <title type =“main”>抽象</ title> >东北亚的新生代的后期中生代涉及太平洋地壳和融合的连续介绍欧亚大陆，北美和Okhotsk海板块。板碰撞的时机对于了解东北亚的构造演变至关重要。在这项研究中，我们专注于俄罗斯远东萨哈林岛的欧亚邦的Okhotsk海底碰撞，这是一个高度争议的问题，特别是关于碰撞时机。为了确定这一碰撞的精确时间，我们从萨哈林岛中向东萨哈林的Zircon U-Pb数据报告Zircon U-Pb数据。来自四个Metaseigatiange Rocks的旨在锆石数据表明，Sikhote-Alin Orentenic带是东萨哈林含量复合物的主要出处。同时，最小的脱喉血管涡流度约束了东萨哈林的最大沉积年龄在49？ma之后。 Langeri和Val'za钚都是由灭菌的S型花岗岩制成的。四个花岗岩样品在36-38mA的36-38mA中产生一致的年龄，表明将两种钚置于中间何中。他们的一代被认为是通过在与欧亚板块碰撞引起的构造增厚之后的下地壳中的较低地壳的地壳肛门的地壳anatexis来源。因此，我们的年龄数据限制了Okhotsk Sea Plate和Euroasia Plate碰撞发生在49到38的中间eocene中。这个年龄范围与萨哈林岛和Okhotsk海中鉴定的后期何种期不合格一致。</ 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9期</span><b style="margin: 0 2px;">|</b><span>共15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=Zhao Pan&option=202" target="_blank" rel="nofollow">Zhao Pan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexandrov Igor&option=202" target="_blank" rel="nofollow">Alexandrov Igor;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jahn Bor‐ming&option=202" target="_blank" rel="nofollow">Jahn Bor‐ming;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ivin Vitaly&option=202" target="_blank" rel="nofollow">Ivin Vitaly;</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 GeosciencesNational Taiwan UniversityTaipei Taiwan;</p> <p>Far East Geological InstituteFar Eastern Branch of the Russian Academy of SciencesVladivostok Russia;</p> <p>Department of GeosciencesNational Taiwan UniversityTaipei Taiwan;</p> <p>Far East Geological InstituteFar Eastern Branch of the Russian Academy of SciencesVladivostok Russia;</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=Okhotsk Sea Plate&option=203" rel="nofollow">Okhotsk Sea Plate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eurasia Plate&option=203" rel="nofollow">Eurasia Plate;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sakhalin Island&option=203" rel="nofollow">Sakhalin Island;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=collision&option=203" rel="nofollow">collision;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=zircon age&option=203" rel="nofollow">zircon age;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=middle Eocene&option=203" rel="nofollow">middle Eocene;</a> </p> <div class="translation"> 机译：Okhotsk Sea Plate;欧亚邦;萨哈林岛;碰撞;锆石年龄;中间eocene; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:24:19</span> </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="/academic-journal-cn_chinese-geology-english_thesis/0201272277380.html">Zircon SHRIMP U-Pb dating of the Neogene coral reefs,Xisha Islands,South China Sea:implications for tectonic evolution</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hong Xu&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hong Xu,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao-peng Ji&option=202" target="_blank" rel="nofollow" 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamamoto Takahiro&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yamamoto Takahiro </a> <span>2016</span> </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：欧亚板块东缘晚白垩世火成岩闪耀发生的时间：日本西南地区相生-有马-科托地区的新锆石U-Pb年龄</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sinica_thesis/0201252707483.html">印度与欧亚两大陆块碰撞时间的厘定:来自锆石SHRIMP U-Pb年龄的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=夏斌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 夏斌</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=林清茶&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,林清茶</a> <a 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