Halogen Heterogeneity in the Lithosphere and Evolution of Mantle Halogen Abundances Inferred From Intraplate Mantle Xenoliths

Kobayashi Masahiro; Sumino Hirochika; Burgess Ray; Nakai Shunichi; Iizuka Tsuyoshi; Nagao Jun; Kagi Hiroyuki; Nakamura Michihiko; Takahashi Eiichi; Kogiso Tetsu; Ballentine Chris J.

摘要

Abstract >We present halogen, noble gas, and major and trace element compositions of mantle xenoliths from intraplate settings (Eifel, Kilbourne Hole, San Carlos, and Hawaii). The xenoliths show a wide range of halogen elemental ratios, which form two arrays centered on the halogen composition of mid‐ocean ridge basalts. The samples on the array toward high I/Cl value have relatively low Cl concentration and low ratios of highly incompatible elements relative to heavy rare earth elements, whereas the samples on the array toward low Br/Cl value have higher Cl concentration and trace elements ratios. The detailed mechanisms to account for these signatures are equivocal at present. However, they are most likely to be related to secondary processes of volatile loss during partial melting and secondary phase formation during interaction with melts. The common primary mid‐ocean ridge basalt‐like halogen ratios in mantle xenoliths from different parts of the globe indicate that the mantle itself must have a relatively uniform composition over a wide scale. The mantle has maintained its halogen composition over billion year timescales without being affected by I‐rich halogens being transported into the mantle. Mass balance calculations suggest that, in order to maintain the I/Cl ratio of the convecting mantle over 2?Gyr, the I/Cl ratio of the subducted halogens must be no more than several times higher than the present‐day mantle value. </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> >我们呈现卤素，贵族气体和主要和微量和痕量元素组合物从内部导流设置（Eifel，Kilbourne孔，San Carlos和Hawaii）。 Xenoliths显示出广泛的卤素元素比率，其形成两个以中海脊玄武岩的卤素组成为中心的阵列。朝向高I / Cl值的阵列上的样品具有相对于重稀土元素的高度不相容元素的Cl浓度和低比率，而阵列朝向低Br / Cl值的样品具有更高的Cl浓度和微量元素比率。占这些签名的详细机制目前是等因素。然而，它们最有可能与在与熔体相互作用期间部分熔化和二次相形成期间的挥发性损失的二次过程。来自全球不同部位的披风XenoLiths中的常见初级中海脊玄武岩卤素率表明，披风本身必须在宽范围内具有相对均匀的组成。地幔在十亿年的时间尺度保持卤素组成，而不会受到富含I的卤素被运输到地幔的影响。质量平衡计算表明，为了保持对流壁龛的I / Cl比2？Gyr，悬漏的卤素的I / Cl比率不超过本日地幔值的几倍。< / 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=Kobayashi Masahiro&option=202" target="_blank" rel="nofollow">Kobayashi Masahiro;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sumino Hirochika&option=202" target="_blank" rel="nofollow">Sumino Hirochika;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Burgess Ray&option=202" target="_blank" rel="nofollow">Burgess Ray;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakai Shunichi&option=202" target="_blank" rel="nofollow">Nakai Shunichi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iizuka Tsuyoshi&option=202" target="_blank" rel="nofollow">Iizuka Tsuyoshi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nagao Jun&option=202" target="_blank" rel="nofollow">Nagao Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kagi Hiroyuki&option=202" target="_blank" rel="nofollow">Kagi Hiroyuki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakamura Michihiko&option=202" target="_blank" rel="nofollow">Nakamura Michihiko;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Takahashi Eiichi&option=202" target="_blank" rel="nofollow">Takahashi Eiichi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kogiso Tetsu&option=202" target="_blank" rel="nofollow">Kogiso Tetsu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ballentine Chris J.&option=202" target="_blank" rel="nofollow">Ballentine Chris J.;</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>Geochemical Research Center Graduate School of ScienceThe University of TokyoTokyo Japan;</p> <p>Department of Basic Science Graduate School of Arts and SciencesThe University of TokyoTokyo Japan;</p> <p>School of Earth and Environmental SciencesThe University of ManchesterManchester UK;</p> <p>Earthquake Research InstituteThe University of TokyoTokyo Japan;</p> <p>Department of Earth and Planetary Science Graduate School of ScienceThe University of TokyoTokyo Japan;</p> <p>Department of Earth and Planetary Science Graduate School of ScienceThe University of TokyoTokyo Japan;</p> <p>Geochemical Research Center Graduate School of ScienceThe University of TokyoTokyo Japan;</p> <p>Department of Earth Science Graduate School of ScienceTohoku UniversitySendai Japan;</p> <p>Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Department of Interdisciplinary Environment Graduate School of Human and Environmental StudiesKyoto UniversityKyoto Japan;</p> <p>Department of Earth SciencesUniversity of OxfordOxford UK;</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=Halogen&option=203" rel="nofollow">Halogen;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mantle xenolith&option=203" rel="nofollow">Mantle xenolith;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lithospheric mantle&option=203" rel="nofollow">Lithospheric mantle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Subcontinental lithospheric mantle&option=203" rel="nofollow">Subcontinental lithospheric mantle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Intraplate setting&option=203" rel="nofollow">Intraplate setting;</a> </p> <div class="translation"> 机译：卤素;地幔Xenolith;岩性地幔;亚丁型岩石罩;腔内设置; </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/0704023360762.html">Halogen Heterogeneity in the Lithosphere and Evolution of Mantle Halogen Abundances Inferred From Intraplate Mantle Xenoliths</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kobayashi Masahiro&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kobayashi Masahiro,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sumino Hirochika&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sumino Hirochika,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Burgess 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href="/academic-journal-cn_journal-graduate-school-chinese-academy-sciences_thesis/0201279649555.html">岩石圈弯曲的黏弹性松弛及其对确定弹性岩石圈厚度的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邵翠法&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 邵翠法</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王世民&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王世民</a> <span> <a href="/journal-cn-3816/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国科学院研究生院学报 </a> </span> <span> . 2020</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-university-chinese-academy-sciences_thesis/0201280652050.html">岩石圈弯曲的黏弹性松弛及其对确定弹性岩石圈厚度的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邵翠法&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 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<span> <a href="/conference-cn-43375/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国矿物岩石地球化学学会第17届学术年会 </a> <span> <span> . 2019</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020315322671.html">中国大陆岩石圈地震体波三维走时速度成像与地震定位研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=莘海亮&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 莘海亮</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120112743060.html">岩石圈构造变形物理模拟实验装置及实验方法</a> <b>[P]</b> . <span> 中国专利： CN112781519A </span> <span> . 2021-05-11</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120113254057.html">基于岩石圈公共数据库的含断裂的三维粘弹性建模方法</a> <b>[P]</b> . <span> 中国专利： CN113298942A </span> <span> . 2021-08-24</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130445877414.html">Light fitting using LV halogen lamp has protective glass cylinder provided with matt mantle surface enclosed by transparent glass body</a> <b>[P]</b> . <span> 外国专利：  DE10101893C1 </span> <span> . 2002-07-04</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LV卤素灯的灯具具有防护玻璃圆柱体，该圆柱体具有被透明玻璃体包围的无光泽罩表面 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130464335372.html">Illumination optics for remission measuring appts. - concentrates light beam from halogen lamp in mantle surfaces and deflects by 45 deg. onto measuring spot</a> <b>[P]</b> . <span> 外国专利：  DE4013421A1 </span> <span> . 1991-10-31</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：照明光学器件，用于缓解测量装置。 -将卤素灯发出的光束会聚在地幔表面，并偏转45度。到测量点 </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;" 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