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首页> 外文期刊>Journal of Metamorphic Geology >Mesozoic to Cenozoic tectono‐metamorphic history of the South Pamir–Hindu Kush (Chitral, NWNW Pakistan): Insights from phase equilibria modelling, and garnet–monazite petrochronology
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Mesozoic to Cenozoic tectono‐metamorphic history of the South Pamir–Hindu Kush (Chitral, NWNW Pakistan): Insights from phase equilibria modelling, and garnet–monazite petrochronology

机译：中生代到新生代构造 - 南方帕米尔 - 印度科什耳诗的变质史（奇克里氏， NW NW Pakistan）：相位均衡建模和石榴石 - 无人岩岩石学的见解

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Abstract > The Karakoram–Hindu Kush–Pamir and adjacent Tibetan plateau belt comprise a series of Gondwana‐derived crustal fragments that successively accreted to the Eurasian margin in the Mesozoic as the result of the progressive Tethys ocean closure. These domains provide unique insights into the thermal and structural history of the Mesozoic to Cenozoic Eurasian plate margin, which are critical to inform the initial boundary conditions (e.g. crustal thickness, structure and thermo‐mechanical properties) for the subsequent development of the large and hot Tibetan–Himalaya orogen, and the associated crustal deformation processes. Using a combination of microstructural analyses, thermobarometry modelling and U–Th–Pb monazite and Lu–Hf garnet geochronology, the study reappraises the metamorphic history of exposed mid‐crustal metapelites in the Chitral region of the South Pamir–Hindu Kush ( <fc>NW</fc> Pakistan). This study also demonstrates that trace elements in monazite (especially Y and Dy), combined with thermodynamical modelling and Lu–Hf garnet dating, provides a powerful integrated toolbox for constraining long‐lived and polyphased tectono‐metamorphic histories in all their spatial and temporal complexity. Rocks from the Chitral region were progressively deformed and metamorphosed at sub‐ and supra‐solidus conditions through at least four distinct episodes from the Mesozoic to the Cenozoic. Rocks were first metamorphosed at ~400–500°C and ~0.3? <fc>GP</fc> a in the Late Triassic–Early Jurassic (210–185?Ma), likely in response to the accretion of the Karakoram during the Cimmerian orogeny. Pressure and temperature subsequently increased by ~0.3?GPa and 100°C in the Early‐ to Mid Cretaceous (140–80?Ma), coinciding with the intrusion of calcalkaline granitic plutons across the Karakoram and </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：ID =“JMG12479-ABS-ABS-0001”XML：Lang =“en”> <标题类型=“main”>抽象</ title> > karakoram-hindu kush-pamir和邻近的西藏高原皮带包括一系列巨大的地壳碎片，即在中生代的欧亚边缘被连续地积累了欧亚人的级数，因为渐进的Thishys海洋关闭。这些域提供了独特的见解，进入中生代欧亚板材边距的中生代的热和结构历史，这对于通知初始边界条件（例如地壳厚度，结构和热机械性能）至关重要，以便随后的大型和热藏喜马拉雅山脉，以及相关的地壳变形过程。使用微观结构分析，热能测量建模和U-TH-PB Monazite和Lu-HF Garnet地理学的组合，研究重新评估了南帕米尔 - 印度教床（<FC> NW </ FC>巴基斯坦）。本研究还表明，Monazite（特别是Y和Dy）中的微量元素与热力学建模和LU-HF Garnet约会相结合，提供了一个强大的集成工具箱，用于在所有空间和时间复杂性中约束长寿命和多相构造 - 变质历史。来自氯离区区域的岩石通过来自中生代的中生代的至少四个不同的发作来逐渐变形和变质。岩石首先在〜400-500°C和〜0.3的〜0.3〜0.3在晚期三叠纪侏罗纪（210-185？mA）中，尤其是在Cimmerian Orogeny期间响应喀喇昆仑的增生。随后，压力和温度随后在早期至中间白垩纪（140-80？mA）中增加〜0.3？GPA和100​​°C，与喀喇昆仑的考角素花岗岩型材的侵入 </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-35076/'>《Journal of Metamorphic Geology》</a> <b style="margin: 0 2px;">|</b><span>2019年第5期</span><b style="margin: 0 2px;">|</b><span>共34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=Soret Mathieu&option=202" target="_blank" rel="nofollow">Soret Mathieu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Larson Kyle P.&option=202" target="_blank" rel="nofollow">Larson Kyle P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cottle John M.&option=202" target="_blank" rel="nofollow">Cottle John M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Smit Matthijs&option=202" target="_blank" rel="nofollow">Smit Matthijs;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Johnson Alex&option=202" target="_blank" rel="nofollow">Johnson Alex;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shrestha Sudip&option=202" target="_blank" rel="nofollow">Shrestha Sudip;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ali Asghar&option=202" target="_blank" rel="nofollow">Ali Asghar;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Faisal Shah&option=202" target="_blank" rel="nofollow">Faisal Shah;</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>Earth and Environmental SciencesUniversity of British Columbia OkanaganKelowna BC Canada;</p> <p>Earth and Environmental SciencesUniversity of British Columbia OkanaganKelowna BC Canada;</p> <p>Department of Earth ScienceUniversity of California Santa BarbaraSanta Barbara California;</p> <p>Earth Ocean &</p> <p>Atmospheric SciencesUniversity of British ColumbiaVancouver BC Canada;</p> <p>Department of Earth ScienceUniversity of California Santa BarbaraSanta Barbara California;</p> <p>Earth and Environmental SciencesUniversity of British Columbia OkanaganKelowna BC Canada;</p> <p>Earth and Environmental SciencesUniversity of British Columbia OkanaganKelowna BC Canada;</p> <p>Earth and Environmental SciencesUniversity of British Columbia OkanaganKelowna BC Canada;</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/165.html" title="地质学">地质学;</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=Lu–Hf garnet geochronology&option=203" rel="nofollow">Lu–Hf garnet geochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mesozoic Eurasian proto‐plateau&option=203" rel="nofollow">Mesozoic Eurasian proto‐plateau;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South Pamir–Hindu Kush&option=203" rel="nofollow">South Pamir–Hindu Kush;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermodynamic modelling&option=203" rel="nofollow">thermodynamic modelling;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=U–Th–Pb monazite petrochronology&option=203" rel="nofollow">U–Th–Pb monazite petrochronology;</a> </p> <div class="translation"> 机译：Lu-HF石榴石地理学;中生代欧亚原型高原;南方帕米尔 - 印度犬;热力学造型;U-TH-PB Monazite Petroronologology; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025659614.html">Mesozoic to Cenozoic tectono‐metamorphic history of the South Pamir–Hindu Kush (Chitral, <fc 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