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Evidence for a Moist to Wet Source Transition Throughout the Oman‐UAE Ophiolite, and Implications for the Geodynamic History

机译：在整个阿曼 - 阿联酋的Ophiolite整个潮湿源过渡的证据，以及对地球动力学历史的影响

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Abstract > The Oman‐United Arab Emirates (UAE) ophiolite represents the largest and best‐preserved fragment of obducted oceanic lithosphere in the world. However, debate continues regarding its geodynamic history. This debate is in part a consequence of the lateral variability in the later stage magmatic units, with arc signatures considered to be well developed in the north of the ophiolite but less so in the south. In this study, we investigate later stage intrusions in the central and southern part of the ophiolite. These intrusions vary from wehrlite to gabbro and tonalite and crosscut all levels of the main ophiolite sequence from the mantle peridotites up to the sheeted dike complex. They are characterized by the presence of magmatic amphibole, low TiO <sub>2</sub> (1?wt%), document an enrichment in Th, Sr, and Ba, depletion of Y and Dy, and decreasing Dy/Yb and Dy/Dy* with increased fractionation. These data record hydrous fractionation with a significant role for amphibole, which is comparable to many arc‐type magmas. The relative Nb and light rare earth element ((La/Yb)n <sub>chon</sub> ??1) depletion and coupled Nd and Hf isotope variations indicate the same (but depleted) Indian mid‐ocean ridge basalts‐type mantle source as the main ophiolite sequence. More radiogenic Pb isotope compositions of plagioclase imply the addition of a fluid component likely derived from sediments or altered oceanic crust. These intrusions occur across larger areas than previously reported, implying the entire ophiolite formed in a setting characterized by arc‐type magmas, such as a suprasubduction zone setting. </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> > 阿曼阿拉伯联合酋长国（阿联酋）Ophiolite代表了世界上最大，最先进的Oconic海洋岩石圈的片段。但是，辩论仍在继续进行地质动力学历史。这场辩论部分是后期舞台单位的横向变异性的结果，认为弧形签名被认为是在眼科北部的北部很好的，但在南方较少。在这项研究中，我们研究了眼科中的中央和南部的后期入侵。这些入侵从Wehrlite到Gabbro和Tonalite和铜的横切，并将所有水平的主要眼磷灰石序列从地幔透过达到片状堤隙络合物。它们的特征在于岩浆阳吡胶，低TIO的存在 <sub> 2 </ sub> （＆ 1？wt％），将富集，y和dy的富集，y和dy的耗尽和dy / yb和dy / dy *的分馏减少。这些数据记录了含水分馏，对锥形阳性作用具有重要作用，这与许多弧型岩浆相当。相对Nb和光稀土元素（（la / yb）n <sub> chon </ sub> α1）耗尽和偶联Nd和Hf同位素变化表示相同的（但耗尽）印度中海脊玄武岩型地幔源作为主要的眼磷酸序列。更多的粘接性Pb同位素组合物的Plagioclase意味着添加可能来自沉积物或改变的海壳的流体组分。这些入侵发生在比以前报道的较大区域上，暗示在以弧形磁带为特征的设置中形成的整个眼镜铝，例如SuprasubDucke区设定。 </ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共22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=Graaff S. J.&option=202" target="_blank" rel="nofollow">Graaff S. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Goodenough K. M.&option=202" target="_blank" rel="nofollow">Goodenough K. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Klaver M.&option=202" target="_blank" rel="nofollow">Klaver M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lissenberg C. J.&option=202" target="_blank" rel="nofollow">Lissenberg C. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jansen M. N.&option=202" target="_blank" rel="nofollow">Jansen M. N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Millar I.&option=202" target="_blank" rel="nofollow">Millar I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Davies G. R.&option=202" target="_blank" rel="nofollow">Davies G. R.;</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>Faculty of ScienceVrije Universiteit AmsterdamAmsterdam Netherlands;</p> <p>British Geological Survey the Lyell CentreEdinburgh UK;</p> <p>School of Earth SciencesUniversity of Bristol Wills Memorial BuildingBristol UK;</p> <p>School of Earth and Ocean SciencesCardiff UniversityCardiff UK;</p> <p>Faculty of ScienceVrije Universiteit AmsterdamAmsterdam Netherlands;</p> <p>British Geological SurveyNottingham UK;</p> <p>Faculty of ScienceVrije Universiteit AmsterdamAmsterdam Netherlands;</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=Oman‐UAE ophiolite&option=203" rel="nofollow">Oman‐UAE ophiolite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ophiolites&option=203" rel="nofollow">ophiolites;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=amphibole fractionation&option=203" rel="nofollow">amphibole fractionation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=major and trace element geochemistry&option=203" rel="nofollow">major and trace element geochemistry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=suprasubduction zone&option=203" rel="nofollow">suprasubduction zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=MELTS&option=203" rel="nofollow">MELTS;</a> </p> <div class="translation"> 机译：阿曼 - 阿联器异丙钛矿;眼光;锥形分馏;主要和痕量元素地球化学;Suprasub区;融化; </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/0704023360757.html">Evidence for a Moist to Wet Source Transition Throughout the Oman‐UAE Ophiolite, and Implications for the Geodynamic History</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Graaff S. 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2012-06-28</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：使用状态转换历史记录防止未经授权访问的资源 </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('0704023360757','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 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