Light Stable Isotopic Compositions of Enriched Mantle Sources: Resolving the Dehydration Paradox

Dixon J. E.; Bindeman I. N.; Kingsley R. H.; Simons K. K.; Le Roux P. J.; Hajewski T. R.; Swart P.; Langmuir C. H.; Ryan J. G.; Walowski K. J.; Wada I.; Wallace P. J.

摘要

Abstract > Volatile and stable isotope data provide tests of mantle processes that give rise to mantle heterogeneity. New data on enriched mid‐oceanic ridge basalts (MORB) show a diversity of enriched components. Pacific PREMA‐type basalts (H <sub>2</sub> O/Ce?=?215?±?30, δD <sub>SMOW</sub> ?=??45?±?5 ‰) are similar to those in the northern Atlantic (H <sub>2</sub> O/Ce?=?220?±?30; δD <sub>SMOW</sub> ?=??30 to ?40 ‰). Basalts with EM‐type signatures have regionally variable volatile compositions. Northern Atlantic EM‐type basalts are wetter (H <sub>2</sub> O/Ce?=?330?±?30) and have isotopically heavier hydrogen (δD <sub>SMOW</sub> ?=??57?±?5 ‰) than northern Atlantic MORB. Southern Atlantic EM‐type basalts are damp (H <sub>2</sub> O/Ce?=?120?±?10) with intermediate δD <sub>SMOW</sub> (?68?±?2 ‰), similar to δD <sub>SMOW</sub> for Pacific MORB. Northern Pacific EM‐type basalts are dry (H <sub>2</sub> O/Ce?=?110?±?20) and isotopically light (δD <sub>SMOW</sub> ?=??94?±?3 ‰). A multistage metasomatic and melting model accounts for the origin of the enriched components by extending the subduction factory concept down through the mantle transition zone, with slab temperature a key variable. Volatiles and their stable isotopes are decoupled from lithophile elements, reflecting primary dehydration of the slab followed by secondary rehydration, infiltration, and re‐equilibration by fluids derived from dehydrating subcrustal hydrous phases (e.g., antigorite) in cooler, deeper parts of the slab. Enriched mantle sources form by addition of 1% carbonated eclogite?±?sediment‐derived C‐O‐H‐Cl fluids to depleted mantle at 180–280 km (EM) or within the transition zone (PREMA). </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”> <标题类型=“main”>抽象</ title> > 挥发性和稳定的同位素数据提供了导致地幔异质性的地幔过程的测试。丰富的中海脊玄武岩（Morb）的新数据显示了丰富的组件的多样性。太平洋Prema型玄武岩（H <sub> 2 </ sub> O / Ce？=？215？±±30，ΔD <sub> smow </ sub> ？= ?? 45？±5次）类似于北大西洋的那些（H. <sub> 2 </ sub> o / ce？=？220？±30; Δd. <sub> smow </ sub> ？= ?? 30到？40‰）。具有EM型签名的玄武岩具有区域可变的挥发性组合物。北大西洋EM型底座是湿润的（H. <sub> 2 </ sub> o / ce？=Δ330？±30）并具有同位素较重的氢气（Δd <sub> smow </ sub> ？= ?? 57？57？±5‰）比北大西洋Morb。南部的大西洋EM型玄武岩是潮湿的（h <sub> 2 </ sub> o / ce？=Δ= 120？±10），中间Δd <sub> smow </ sub> （？68？68？±2‰），类似于Δd <sub> smow </ sub> 对于太平洋Morb。北太平洋EM型玄武岩干燥（H. <sub> 2 </ sub> O / Ce？=？110？±20）和同位素光（ΔD <sub> smow </ sub> ？= ?? 94？±3‰）。多级态态和熔化模型通过将俯冲工厂概念延伸通过披风过渡区域来延伸俯冲工厂概念，使平板温度成为钥匙变量。挥发物和它们的稳定同位素由鳞片内元件分离，反射平板的初级脱水，然后通过衍生自脱水的乳湿阶段（例如，抗真菌）在冷却器的较深部分的脱水的流体进行次级再水化，渗透和重新平衡。通过加入碳酸味肠（碳酸庚酸盐蛋白αα）富含甲状裸物流源形式，沉积物衍生的C-O-H-C1流体，以在180-280km（EM）或过渡区（PREMA）内耗尽披肩。 </ 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>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共39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=Dixon J. E.&option=202" target="_blank" rel="nofollow">Dixon J. E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bindeman I. N.&option=202" target="_blank" rel="nofollow">Bindeman I. N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kingsley R. H.&option=202" target="_blank" rel="nofollow">Kingsley R. H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Simons K. K.&option=202" target="_blank" rel="nofollow">Simons K. K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Le Roux P. J.&option=202" target="_blank" rel="nofollow">Le Roux P. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hajewski T. R.&option=202" target="_blank" rel="nofollow">Hajewski T. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Swart P.&option=202" target="_blank" rel="nofollow">Swart P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Langmuir C. H.&option=202" target="_blank" rel="nofollow">Langmuir C. H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ryan J. G.&option=202" target="_blank" rel="nofollow">Ryan J. G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Walowski K. J.&option=202" target="_blank" rel="nofollow">Walowski K. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wada I.&option=202" target="_blank" rel="nofollow">Wada I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wallace P. J.&option=202" target="_blank" rel="nofollow">Wallace P. 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>College of Marine ScienceUniversity of South FloridaSt. Petersburg FL USA;</p> <p>Department of Earth SciencesUniversity of OregonEugene OR USA;</p> <p>Graduate School of OceanographyUniversity of Rhode IslandNarragansett RI USA;</p> <p>Exxon‐MobilHouston TX USA;</p> <p>Department of Geological SciencesUniversity of Cape TownRondebosch South Africa;</p> <p>Department of GeologyUniversity of MiamiMiami FL USA;</p> <p>Division of Marine Geology and Geophysics Rosenstiel School of Marine and Atmospheric ScienceUniversity of MiamiMiami FL USA;</p> <p>Department of Earth and Planetary ScienceHarvard UniversityCambridge MA USA;</p> <p>School of GeosciencesUniversity of South FloridaTampa FL USA;</p> <p>Department of Earth SciencesUniversity of OregonEugene OR USA;</p> <p>Department of Earth SciencesUniversity of MinnesotaMinneapolis MN USA;</p> <p>Department of Earth SciencesUniversity of OregonEugene OR USA;</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=volatiles&option=203" rel="nofollow">volatiles;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=stable isotopes&option=203" rel="nofollow">stable isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle geochemistry&option=203" rel="nofollow">mantle geochemistry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction&option=203" rel="nofollow">subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=metasomatism&option=203" rel="nofollow">metasomatism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic basalt&option=203" rel="nofollow">oceanic basalt;</a> </p> <div class="translation"> 机译：挥发物;稳定同位素;地球化学;俯冲;弥扑玄武岩;海洋玄武岩; </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/0704023360554.html">Light Stable Isotopic Compositions of Enriched Mantle Sources: Resolving the Dehydration Paradox</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dixon J. 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rel="nofollow" class="tuijian_authcolor"> . 四川水利 </a> </span> <span> . 2016</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_sichuan-water-power_thesis/0201215284440.html">吉牛水电站引水隧洞富含云母岩体导致施工降效索赔的探讨</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=汪征&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 汪征</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邢俊敏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,邢俊敏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李忠历&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李忠历</a> <span> <a href="/journal-cn-9737/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 四川水力发电 </a> </span> <span> . 2014</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_sichuan-water-power_thesis/0201215295270.html">吉牛水电站富含云母岩体引水隧洞爆破施工技术</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘涛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘涛</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=何承俊&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,何承俊</a> <span> <a href="/journal-cn-9737/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 四川水力发电 </a> </span> <span> . 2013</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_sichuan-water-power_thesis/0201215295556.html">富含云母岩体隧洞开挖爆破技术</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=段会平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 段会平</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王志强&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王志强</a> <span> <a href="/journal-cn-9737/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 四川水力发电 </a> </span> <span> . 2013</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-14636_thesis/020221196056.html">三元复合驱后富含粘土的脱水破乳剂的研制与应用</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=付亚荣&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 付亚荣</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李洪江&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李洪江</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=邓桃&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,邓桃</a> <span> <a href="/conference-cn-14636/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2009中国油田化学品发展研讨会（第23次全国工业表面活性剂发展研讨会） </a> <span> <span> . 2009</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020313965020.html">富含瓦斯煤岩体采掘失稳非线性力学机理研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张天军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张天军</a> <span> . 2009</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120894538.html">富含同位素的氢化硼化合物的合成方法以及富含同位素的硼烷的合成方法</a> <b>[P]</b> . <span> 中国专利： CN101001829B </span> <span> . 2012.02.22</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120105204472.html">富含同位素的氢化硼化合物的合成方法以及富含同位素的硼烷的合成方法</a> <b>[P]</b> . <span> 中国专利： CN101001829A </span> <span> . 2007-07-18</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130402374058.html">Carbon monoxide stable isotope enrichment apparatus and carbon monoxide stable isotope enrichment method</a> <b>[P]</b> . <span> 外国专利：  JP6606522B2 </span> <span> . 2019-11-13</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：一氧化碳稳定同位素富集装置和一氧化碳稳定同位素富集方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130438908044.html">Composition for topical application to keratinic matter, especially hair, comprises compound enriched in at least one stable non-radioactive isotope of element having at least two natural non-radioactive isotopes</a> <b>[P]</b> . <span> 外国专利：  FR2867385A1 </span> <span> . 2005-09-16</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: 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