Mantle Lithosphere Rheology, Vertical Tectonics, and the Exhumation of (U)HP Rocks

机译：地幔岩石圈流变学，垂直构造，以及（U）HP岩石的挖掘

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Abstract >Numerical modeling results indicate that mantle lithosphere rheology can influence the pressure‐temperature‐time (P‐T‐t) trajectories of continental crust subducted and exhumed during the onset of continental collision. Exhumation of ultrahigh‐pressure (~35?kbar)/high‐temperature (~750°C) metamorphic rocks is more prevalent in models with stronger continental mantle lithosphere (e.g., dry), whereas high‐pressure (~9–22?kbar)/low‐temperature (350°C–630°C) metamorphic rocks occur in models with weaker rheology (e.g., hydrated) for the same layer. In the latter case, the buried crustal rocks can remain encased in ablatively subducting mantle lithosphere, reach only moderate temperatures, and exhume by dripping/detachment of the lithospheric root. In this transition from subduction to a dripping style of “vertical tectonics,” burial and exhumation of crustal rocks are driven without imposed far‐field plate convergence. The model results are compared against thermobarometric P‐T estimates from major (ultra)high‐pressure metamorphic terranes. We propose that the exhumation of high‐pressure/low‐temperature metamorphic rocks in Tav?anl? and Afyon zones in western Anatolia may be caused by viscous dripping of mantle lithosphere suggesting a weaker continental mantle lithosphere, whereas (ultra)high‐pressure exhumation (e.g., Dabie Shan‐eastern China and Dora Maira‐western Alps) may be associated with plate‐like subduction. In the latter case, the slab is much stronger and deformation is localized to the subduction interface along which rocks are buried to >100?km depth before they are exhumed to the near surface. </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”> <标题类型=“main”>抽象</ title> >数值建模结果表明，地幔岩石圈流变可以影响压力温度 - 时间（p- T-T）大陆碰撞期间陆地地壳的轨迹塌陷和挖掘。超高压（〜35？kbar）/高温（〜750°C）变质岩石的展示在欧式地幔岩石圈（例如干）更强的型号中更为普遍，而高压（〜9-22？kbar ）/低温（350°C-630℃）变质岩石发生在具有较弱的流变学（例如，水合）的模型中进行相同层。在后一种情况下，掩埋的地壳岩石可以在嗜锅底板岩石圈中留下来封装，仅达到中等温度，通过岩石术根的剥离/脱离呼吸。在这种从俯冲转变为“垂直构造的滴度样式”，在没有施加的远场融合的情况下驱动地壳岩石的埋葬和挖掘。将模型结果与来自主要（超）高压变质陶器的热磁化物P-T估计进行比较。我们建议在TAV的高压/低温变质岩石挖掘？ANL？阿纳托利亚西部的AFYON区可能是由岩石圈的粘性滴落引起的岩石圈，表明较弱的大陆地幔岩石圈，而（超）高压挖掘（例如，Dabie Shan-Eastern China和Dora Maira-Western Alps）可能与板块相关联 - 般的俯冲。在后一种情况下，板坯更强大，变形是局部化的，岩体沿着该俯冲界面埋在岩体上，岩石被埋到于> 100？Km深度，然后送到近表面。</ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共16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=Bodur ?mer F.&option=202" target="_blank" rel="nofollow">Bodur ?mer F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=G??ü? O?uz H.&option=202" target="_blank" rel="nofollow">G??ü? O?uz H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pysklywec Russell N.&option=202" target="_blank" rel="nofollow">Pysklywec Russell N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Okay Aral I.&option=202" target="_blank" rel="nofollow">Okay Aral I.;</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>Eurasia Institute of Earth SciencesIstanbul Technical UniversityIstanbul Turkey;</p> <p>Eurasia Institute of Earth SciencesIstanbul Technical UniversityIstanbul Turkey;</p> <p>Department of Earth SciencesUniversity of TorontoToronto Ontario Canada;</p> <p>Eurasia Institute of Earth SciencesIstanbul Technical UniversityIstanbul Turkey;</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(HP) exhumation&option=203" rel="nofollow">U(HP) exhumation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=vertical tectonics&option=203" rel="nofollow">vertical tectonics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle lithosphere rheology&option=203" rel="nofollow">mantle lithosphere rheology;</a> </p> <div class="translation"> 机译：U（HP）挖掘;垂直构造;地幔岩石圈流变学; </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/0704025592033.html">Mantle Lithosphere Rheology, Vertical Tectonics, and the Exhumation of (U)HP Rocks</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bodur ?mer F.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bodur ?mer F.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=G??ü? 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Näf,</a> <span>-1</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：具有粘塑性流变学的地幔对流模型中稳定岩石圈中脊的形成</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000131248733.html">Different PT paths recorded in a tectonic mélange (Voltri Massif, NW Italy): implications for the exhumation of HP rocks</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Laura Federico&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Laura Federico,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Laura Crispini&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Laura Crispini,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marco Scambelluri&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Marco Scambelluri,</a> <span>2007</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：在构造的Mélange（Voltri Massif，NW意大利）中记录的不同PT路径：对HP Rocks挖掘的影响</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_nasa_thesis/02071375387.html">Rheology, tectonics, and the structure of the Venus lithosphere</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zuber, M. 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METHOD OF CONSTRUCTION AND USE OF MODELS tectonic seismic zones in the continental lithosphere EARTH</a> <b>[P]</b> . <span> 外国专利：  RU2013116281A </span> <span> . 2014-10-20</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：地球大陆岩石圈地震带的构造模型。大陆岩石圈地球构造地震带模型的构建和使用方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130461878793.html">METHOD OF DETECTING LOCAL CHANGES IN LITHOSPHERE STRESS IN PARTICULAR IN ORDER TO FORECAST TECTONIC TREMORS</a> <b>[P]</b> . <span> 外国专利：  PL290309A1 </span> <span> . 1992-12-14</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：检测岩石球应力局部变化的方法，以预测构造性残余 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130439126515.html">DEVICE FOR MODELLING PRECESSION OF LITHOSPHERE AROUND PLANETARY MANTLE</a> <b>[P]</b> . <span> 外国专利：  RU2263974C2 </span> <span> . 2005-11-10</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：岩石球环绕行星幔模型预测的装置 </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('0704025592033','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 class="journal-sub"> <h2>期刊订阅</h2> <img 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