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首页> 外文期刊>Journal of Metamorphic Geology >Tectonometamorphic evolution of the Atbashi high‐ PP units (Kyrgyz CAOBCAOB , Tien Shan): Implications for the closure of the Turkestan Ocean and continental subduction–exhumation of the South Kazakh continental margin
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Tectonometamorphic evolution of the Atbashi high‐ PP units (Kyrgyz CAOBCAOB , Tien Shan): Implications for the closure of the Turkestan Ocean and continental subduction–exhumation of the South Kazakh continental margin

机译：atbashi高 p p单位（kygyz caob caob，tien shan）：对南哈萨克大陆边缘的南哈萨克大陆挖掘的南哈萨克大陆边缘的关闭影响

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Abstract > The South Tien Shan ( <fc>STS</fc> ) belt results from the last collision event in the western Central Asian Orogenic Belt ( <fc>CAOB</fc> ). Understanding its formation is of prime importance in the general framework of the <fc>CAOB</fc> . The Atbashi Range preserves high‐ P (HP) rocks along the STS suture, but still, its global metamorphic evolution remains poorly constrained. Several <fc>HP</fc> units have been identified: (a) a HP tectonic mélange including boudins of mafic eclogites in a sedimentary matrix, (b) a large (100?km long) high‐ P metasedimentary unit ( <fc>HPMU</fc> ) and (c) a lower blueschist facies accretionary prism. Raman Spectroscopy on carbonaceous material combined with phengite and chlorite multiequilibria and isochemical phase diagram modelling indicates that the <fc>HPMU</fc> recorded homogeneous P–T conditions of 23–25?kbar and 560–570°C along the whole unit. 40 Ar/ 39 Ar dating on phengite from the <fc>HPMU</fc> ranges between 328 and 319?Ma at regional scale. These ages are interpreted as (re‐) crystallization ages of phengite during T <sub>max</sub> conditions at a pressure range of 20–25?kbar. Thermobarometry on samples from the HP tectonic mélange provides similar metamorphic peak conditions. Thermobarometry on the blueschist to lower greenschist facies accretionary prism indicates that it underwent P–T conditions of 5–6?kbar and 290–340°C, highlighting a 17–20?kbar pressure gap between the <fc>HPMU</fc> ‐tectonic </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 xmlns =“http://www.wiley.com/namespaces/wiley”type =“main”xml：id =“jmg12423-abs-abs-0001”xml：lang =“en”> <标题类型=“main” >摘要</ title> >南部山（<fc> sts </ fc>）带来的中央亚洲眶带（<fc> caob </ fc>）的最后一个碰撞事件。了解其形成在<FC> CAOB </ FC>的一般框架中是一个重要的重要性。 atbashi范围沿着STS缝合线储存高 - P </ i>（HP）岩石，但仍然，其全球变质演变仍然受到严重的限制。已经确定了几个<FC> HP </ FC>单位：（a）HP构造Mémange，包括沉积基质中的MAFIC Eclogites的Boudins，（b）大（＆100Ωmh长）高 - p MEDASEDALY单位（<FC> HPMU </ FC>）和（c）下蓝布师相吸收棱镜。碳质材料上的拉曼光谱与磷酸盐和氯酸盐多功能和等级相位图建模结合，表明<Fc> HPMU </ Fc>记录的均匀性 P-T </ i>条件为23-25？Kbar和560-570 °C沿整个单位。 <SUP> 40 </ sup> AR / <SUP> 39 </ SUP> AR在区域范围内从<FC> HPMU </ FC>范围之间进行约会，从328到319？mA之间。这些时代被解释为（重新）在 T </ i> <sub> Max </ sub>条件下在20-25Ω·kbar的条件下解释为phengite的结晶年龄。 HP构造Mélange的样品上的热磁化机提供了类似的变质峰条件。在布鲁斯基师上的热磁化机率为降低绿色蛋白面相吸收棱镜表明它介绍了5-6Ω·kbar和290-340°C的 p-t </ i>条件，突出了17-20？Kbar压力差距< FC> HPMU </ FC> -2-clectonic </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>2018年第8期</span><b style="margin: 0 2px;">|</b><span>共27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=Loury Chloé&option=202" target="_blank" rel="nofollow">Loury Chloé;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rolland Yann&option=202" target="_blank" rel="nofollow">Rolland Yann;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guillot Stéphane&option=202" target="_blank" rel="nofollow">Guillot Stéphane;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lanari Pierre&option=202" target="_blank" rel="nofollow">Lanari Pierre;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ganino Clément&option=202" target="_blank" rel="nofollow">Ganino Clément;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Melis Raphael&option=202" target="_blank" rel="nofollow">Melis Raphael;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jourdon Anthony&option=202" target="_blank" rel="nofollow">Jourdon Anthony;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Petit Carole&option=202" target="_blank" rel="nofollow">Petit Carole;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Beyssac Olivier&option=202" target="_blank" rel="nofollow">Beyssac Olivier;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gallet Sylvain&option=202" target="_blank" rel="nofollow">Gallet Sylvain;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Monié Patrick&option=202" target="_blank" rel="nofollow">Monié Patrick;</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>Université C?te d'AzurValbonne France;</p> <p>Université C?te d'AzurValbonne France;</p> <p>Univ. Grenoble AlpesGrenoble France;</p> <p>Institute of Geological SciencesUniversity of BernBern Switzerland;</p> <p>Université C?te d'AzurValbonne France;</p> <p>Université C?te d'AzurValbonne France;</p> <p>Université C?te d'AzurValbonne France;</p> <p>Université C?te d'AzurValbonne France;</p> <p>Institut de Minéralogie de Physique des Matériaux et de Cosmochimie (IMPMC)Sorbonne Universités – UPMC Univ Paris 06Paris France;</p> <p>Université C?te d'AzurValbonne France;</p> <p>Géosciences MontpellierUMR 5243Montpellier France;</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=Central Asian Orogenic Belt&option=203" rel="nofollow">Central Asian Orogenic Belt;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=continental subduction&option=203" rel="nofollow">continental subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=HP metamorphism&option=203" rel="nofollow">HP metamorphism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P – T – t history&option=203" rel="nofollow">P – T – t history;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=South Tien Shan&option=203" rel="nofollow">South Tien Shan;</a> </p> <div class="translation"> 机译：中亚造山带;大陆俯冲;惠普变质;P - T - T历史;南天山; </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/0704025659402.html">Tectonometamorphic evolution of the Atbashi high‐ <i xmlns="http://www.wiley.com/namespaces/wiley">PP units (Kyrgyz <fc xmlns="http://www.wiley.com/namespaces/wiley">CAOB</fc>CAOB , Tien Shan): Implications for the closure of the Turkestan Ocean and continental subduction–exhumation of the South Kazakh continental margin</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Loury Chloé&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Loury Chloé,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rolland Yann&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rolland Yann,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guillot Stéphane&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Guillot Stéphane,</a> <a href="/journal-foreign-35076/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Metamorphic Geology .</a> <span>2018</span><span>,第8期</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：atbashi高<i xmlns =“http://www.wiley.com/namespaces/wiley”> p </ i> p单位（kygyz <fc xmlns =“http://www.wiley.com /命名空间/ wiley“> caob </ fc> caob，tien shan）：对南哈萨克大陆边缘的南哈萨克大陆挖掘的南哈萨克大陆边缘的关闭影响</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025659526.html">Scales of deformation partitioning during exhumation in a continental subduction channel: A petrofabric study of eclogites and gneisses from <fc xmlns="http://www.wiley.com/namespaces/wiley">NW</fc>NW Spain (Malpica‐Tui Allochthonous Complex)</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Puelles P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Puelles P.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ábalos B.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">ábalos B.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gil Ibarguchi J. 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