• 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Journal of Metamorphic Geology >High‐pressure metamorphic evolution of eclogite and associated metapelite from the Chuacús complex (Guatemala Suture Zone): Constraints from phase equilibria modelling coupled with Lu‐Hf and U‐Pb geochronology
【24h】

High‐pressure metamorphic evolution of eclogite and associated metapelite from the Chuacús complex (Guatemala Suture Zone): Constraints from phase equilibria modelling coupled with Lu‐Hf and U‐Pb geochronology

机译：Chuacús综合体（危地马拉缝合区）eClogite和相关元桥的高压变质演变：相均衡建模的约束与Lu-HF和U-Pb地理学

获取原文
获取原文并翻译 | 示例
           
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

Abstract > As is common in suture zones, widespread high‐pressure rocks in the Caribbean region reached eclogite facies conditions close to ultrahigh‐pressure metamorphism. Besides eclogite lenses, abundant metapelitic rocks in the Chuacús complex (Guatemala Suture Zone) also preserve evidence for high‐pressure metamorphism. A comprehensive petrological and geochronological study was undertaken to constrain the tectonometamorphic evolution of eclogite and associated metapelite from this area in central Guatemala. The integration of field and petrological data allows the reconstruction of a previously unknown segment of the prograde P–T path and shows that these contrasting rock types share a common high‐pressure evolution. An early stage of high‐pressure/low‐temperature metamorphism at 18–20?kbar and 530–580°C is indicated by garnet core compositions as well as the nature and composition of mineral inclusions in garnet, including kyanite–jadeite–paragonite in an eclogite, and chloritoid–paragonite–rutile in a pelitic schist. Peak high‐pressure conditions are constrained at 23–25?kbar and 620–690°C by combining mineral assemblages, isopleth thermobarometry and Zr‐in‐rutile thermometry. A garnet/whole‐rock Lu‐Hf date of 101.8?±?3.1?Ma in the kyanite‐bearing eclogite indicates the timing of final garnet growth at eclogite facies conditions, while a Lu‐Hf date of 95.5?±?2.1?Ma in the pelitic schist reflects the average age of garnet growth spanning from an early eclogite facies evolution to a final amphibolite facies stage. Concordant U‐Pb <fc>LA</fc> ‐ <fc>ICP</fc> ‐ <fc>MS</fc> zircon data from the pelitic schist, in contrast, yield a mean age of 74.0?±?0.5?Ma, which is equivalent to a U‐Pb monazite </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 =“jmg12285-abs-abs-0001”xml：lang =“en”> <标题类型=“main” >摘要</ title> >在缝合区域中常见，加勒比地区的广泛高压岩石达到靠近超高压变质的欧洲植物面部条件。除eClogite镜片外，Chuacús复合物（危地马拉缝线区）中的丰富的元岩也保留了高压变质的证据。采取了全面的岩石和地质学研究，以限制危地马拉中部地区欧洲庚池和相关元桥的元素萌发。字段和岩石数据的整合允许重建先前未知的促进段 p-t </ i>路径，并表明这些对比岩石类型共享普通的高压演化。高压/低温变质的早期阶段为18-20？KBAR和530-580°C，并由石榴石核心组合物表明，石榴石中的矿物质夹杂物的性质和组成，包括kyanite-ydeate-玻璃体在鹈鹕分离的eNlogite和Chloritoid-玻璃体金红石。峰值高压条件通过组合矿物组合，甲呈Isopleth热磁化法和Zr型熔丝体积测定在23-25℃和620-690℃下约束。石榴石/全岩石LU-HF日期为101.8？在Pelitic Sc​​hist中，反映了从早期Eclogite面部进化到最终的倒置的面部阶段的石榴石增长的平均年龄。协调U-PB <FC> LA </ FC> - <FC> ICP </ FC> - <FC> MS </ FC> ZIRCON数据来自PELITE SCIST，相反，产生平均年龄为74.0？±0.5 ？MA，它相当于U-PB Monazite </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1期</span><b style="margin: 0 2px;">|</b><span>共30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=Maldonado Roberto&option=202" target="_blank" rel="nofollow">Maldonado Roberto;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Weber Bodo&option=202" target="_blank" rel="nofollow">Weber Bodo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ortega‐Gutiérrez Fernando&option=202" target="_blank" rel="nofollow">Ortega‐Gutiérrez Fernando;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Solari Luigi A.&option=202" target="_blank" rel="nofollow">Solari Luigi A.;</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>Instituto de GeologíaUniversidad Nacional Autónoma de MéxicoMéxico D.F Mexico;</p> <p>Departamento de GeologíaCentro de Investigación Científica y de Educación Superior de EnsenadaEnsenada B.C Mexico;</p> <p>Instituto de GeologíaUniversidad Nacional Autónoma de MéxicoMéxico D.F Mexico;</p> <p>Centro de GeocienciasUniversidad Nacional Autónoma de MéxicoQuerétaro Mexico;</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=Chuacús complex&option=203" rel="nofollow">Chuacús complex;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guatemala Suture Zone&option=203" rel="nofollow">Guatemala Suture Zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=high‐pressure metamorphism&option=203" rel="nofollow">high‐pressure metamorphism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lu‐Hf and U‐Pb geochronology&option=203" rel="nofollow">Lu‐Hf and U‐Pb geochronology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=phase equilibria modelling&option=203" rel="nofollow">phase equilibria modelling;</a> </p> <div class="translation"> 机译：Chuacús复合体;危地马拉缝合区;高压变质;Lu-HF和U-PB地理学;相平衡建模; </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/0704025659534.html">High‐pressure metamorphic evolution of eclogite and associated metapelite from the Chuacús complex (Guatemala Suture Zone): Constraints from phase equilibria modelling coupled with Lu‐Hf and U‐Pb geochronology</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Maldonado Roberto&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Maldonado Roberto,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Weber Bodo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Weber Bodo,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ortega‐Gutiérrez Fernando&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ortega‐Gutiérrez Fernando,</a> <a href="/journal-foreign-35076/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Metamorphic Geology .</a> <span>2018</span><span>,第1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：Chuacús综合体（危地马拉缝合区）eClogite和相关元桥的高压变质演变：相均衡建模的约束与Lu-HF和U-Pb地理学</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704014673871.html">Metamorphic evolution of lawsonite eclogites from the southern Motagua fault zone, Guatemala: Insights from phase equilibria and Raman spectroscopy</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Endo S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Endo S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wallis S.R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wallis S.R.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tsuboi M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tsuboi M.,</a> <a href="/journal-foreign-35076/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Metamorphic Geology .</a> <span>2012</span><span>,第2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：来自危地马拉南部Motagua断裂带的钠钙榴石榴辉岩的变质演化：相平衡和拉曼光谱的见解</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sinica-english-edition_thesis/0201253301928.html">Differential Evolution of High-Pressure and Ultrahigh-Pressure Metapelites from Habutengsu, Chinese Western Tianshan: Phase Equilibria Modelling and 40Ar/39Ar Geochronology</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=L(U) Zeng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">L(U) Zeng,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ZHANG Lifei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">ZHANG Lifei </a> <a href="/journal-foreign-4923/" target="_blank" rel="nofollow" class="tuijian_authcolor">地质学报（英文版） .</a> <span>2016</span><span>,第002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：中国天山西部哈布滕苏高压与超高压变质岩的差异演化：相平衡模型和40Ar / 39Ar年代学</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_international-workshop-tethyan-orogenesis-metallogeny-asia_thesis/020512192955.html">Zircon U-Pb geochronology, whole-rock geochemical and Lu-Hf isotopic constraints on the petrogenesis of highly evolved I-type rhyolites in the Loei fold belt and their tectonic implications</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tianyu Zhao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tianyu Zhao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Qinglai Feng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Qinglai Feng </a> <a href="/conference-foreign-33462/" target="_blank" rel="nofollow" class="tuijian_authcolor">International Workshop on Tethyan Orogenesis and Metallogeny in Asia and Cooperation among Institutions of Higher Education: Extended Abstract Volume .</a> <span>2014</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：锆石U-Pb地质年代学，全岩地球化学和Lu-Hf同位素约束黎府褶皱带中高度演化的I型流纹岩的岩石成因及其构造意义</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/0206197584.html">Tectonic Evolution of the Izmir-Ankara Suture Zone in Northwest Turkey using Zircon U-Pb Geochronology and Zircon Lu-Hf Isotopic Tracers</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Campbell, Clay Franklin.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Campbell, Clay Franklin. </a> <span>2017</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：锆石U-Pb年代学和锆石Lu-Hf同位素示踪剂在土耳其西北部伊兹密尔-安卡拉缝合带的构造演化</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000132399318.html">TECTONIC EVOLUTION OF THE IZMIR ANKARA SUTURE ZONE IN NORTHWEST TURKEY USING ZIRCON U-PB GEOCHRONOLOGY AND ZIRCON LU-HF ISOTOPIC TRACERS</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Clay Campbell&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Clay Campbell,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Michael Taylor&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Michael Taylor,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Alexis Licht&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Alexis Licht,</a> <span>2017</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：西北土耳其伊兹密尔安卡拉缝合区的构造演变使用锆石U-PB地理学和锆石路易同位素示踪剂</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('0704025659534','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 src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p class="current">目前支持订阅全部北京大学中文核心（2020）期刊目录。</p> <div style="display: flex;margin-top: 69px;justify-content: space-between;"> <div class="no-sub" onclick="$('.journalsub-pop-up').hide()">暂不订阅</div> <div class="other-sub" onclick="continueSub('from=pc-detail')">继续订阅其他期刊</div> </div> </div> </div> <div class="right_btn"> <ul> <li class="gouwuche"> <!-- <a href="javascript:void(0);" onclick="link_analysis('/shoppingcart/auth/list.html',this)">购物车</a>--> </li> <li class="yijian"> <a href="javascript:void(0);" onclick="link_analysis('/mycenter/auth/complaint.html',this)">意见反馈</a> </li> <li class="top"> <a href="javascript:scrollTo(0,0);">回到顶部</a> </li> <li class="shouye"> <a href="/">回到首页</a> </li> </ul> </div> <div class="xllindexfooter"> <div class="xllindexfootercenter"> <div class="xllindexfooterleft left" > <div class="xllindexfooterleftli"> <ul> <li><a href="/about.html">关于掌桥</a></li> <li><a href="/help/helpmap.html">资源导航</a></li> <li><a href="/help/helpguide.html">新手指南</a></li> <li><a href="/help/helpcenter.html">常见问题</a></li> <li><a href="/sitemap.html">网站地图</a></li> <li><a href="/help/helpcenter.html?type=9">版权声明</a></li> </ul> </div> <div class="xllindexfooterleft"> <p class="xllindexfooterlefteamil">客服邮箱：kefu@zhangqiaokeyan.com</p> <div class="xllindexfooterlefttcp"> <div class="xllindexfooterpoliceiimg"></div> <div class="xllindexfooterpoliceispan"> <span>京公网安备：11010802029741号 </span> <span>ICP备案号：<a href="https://beian.miit.gov.cn" rel="nofollow" target="_blank">京ICP备15016152号-6</a></span> <span>六维联合信息科技 (北京) 有限公司©版权所有</span> </div> </div> </div> </div> <div class="xllindexfooterright left"> <ul> <li> <p style="font-weight: bold;">客服微信</p> <div></div> </li> <li> <p style="font-weight: bold;">服务号</p> <div></div> </li> </ul> </div> </div> </div> <span id="0704025659534down" data-source="7," data-out-id="dcPyf/TmYRRC/WmzIliV/g==," data-f-source-id="7" data-title="High‐pressure metamorphic evolution of eclogite and associated metapelite from the Chuacús complex (Guatemala Suture Zone): Constraints from phase equilibria modelling coupled with Lu‐Hf and U‐Pb geochronology" data-price="20" data-site-name="" data-transnum="24" style="display:none;"></span> <input type="hidden" value="4" id="sourcetype"> <input type="hidden" value="35076" id="journalid"> <input type="hidden" value="1" id="inyn_provide_service_level"> <input type="hidden" value="https://cdn.zhangqiaokeyan.com" id="imgcdn"> <input type="hidden" value="1" id="isdeatail"> <input type="hidden" value="" id="syyn_indexed_database"> <input type="hidden" value="" id="servicetype"> <input type="hidden" id="pagename" value="High‐pressure metamorphic evolution of eclogite and associated metapelite from the Chuacús complex (Guatemala Suture Zone): Constraints from phase equilibria modelling coupled with Lu‐Hf and U‐Pb geochronology"/> <input type="hidden" value="thesis_get_original" id="pageIdentification"> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery-1.12.4.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/lwlh_ajax.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zq.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery.cookie.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/top.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.7.7"></script> <script type="text/javascript" src="https://www.zhangqiaokeyan.com/statistics/static/pagecollection.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/tj.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/pushbaidu.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/history.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/util/cookie.js?v=5.7.7"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.7.7"></script> </body> <script> $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); var inyn_provide_service_level = $("#inyn_provide_service_level").val(); if((sourcetype ==1||sourcetype==4)&&inyn_provide_service_level!=4){ getJournal(); } }) </script> </html>