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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe
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Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe

机译：由熔融岩体反应引起的地幔Zn同位素异质性：来自富含Feb的橄榄石和辉兴的证据来自波希米亚群岛，中欧

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Abstract > To investigate the effect of melt‐rock reaction on Zn isotope fractionation and mantle Zn isotopic heterogeneity, we analyzed Zn isotopic compositions of peridotites, pyroxenites, and mineral separates from the Bohemian Massif, Central Europe. The Mg‐lherzolites (Mg#?=?90.9 to 89.1, FeO T ?=?7.9 to 9.0?wt?%) are melting residues with only moderate metasomatism and have δ 66 Zn from 0.11 to 0.20‰. In contrast, the Fe‐rich peridotites (Mg#?=?88.2 to 80.3, FeO T ?=?10.0 to 14.5?wt?%) and pyroxenites have larger ranges of δ 66 Zn from 0.11 to 0.31‰ and ?0.33 to 0.42‰, respectively. Large disequilibrium intermineral Zn isotope fractionation occurs in the Fe‐rich peridotites and pyroxenites with Δ 66 Zn <sub>Opx‐Ol</sub> ?=??0.50‰, Δ 66 Zn <sub>Grt‐Ol</sub> ?=??0.55 to ?0.39‰, Δ 66 Zn <sub>Grt‐Opx</sub> ?=??0.28 to ?0.05‰, and Δ 66 Zn <sub>Grt‐Cpx</sub> ?=??0.50 to 0.12‰. Combined with their low SiO <sub>2</sub> contents and radiogenic Sr‐Nd‐Os isotopic compositions, the high δ 66 Zn of the Fe‐rich peridotites is attributed to reaction between Mg‐lherzolites and percolating SiO <sub>2</sub> ‐undersaturated basaltic melts that incorporated isotopically heavy crustal components. Crystallization of the isotopically heavy percolating melts migrating through the lithospheric mantle yield the high‐δ 66 Zn pyroxenites. The low δ 66 Zn of the pyroxenites and large intermineral Zn isotopic disequilibrium may result from kinetic Zn is </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”>摘要</标题> >探讨熔融岩反应对Zn同位素分级和裂缝Zn同位素异质性的影响，我们分析了来自中欧波希米亚群众的恒星，辉曲苷和矿物分离的Zn同位素组成。 Mg-lorzolites（Mg＃？= 90.9至89.1，Feo t </ sup>？=α.7.9至9.0？wt？％）熔融残留物，仅具有中等的弥言，并且具有δ 66 </ Sup> Zn从0.11到0.20‰。相比之下，Fe富含Fe的苯（Mg＃？= 88.2至80.3，Feo T </ sup>？= 10.0至14.5？wt？％）和Pyroxenites的δ 66 < / sup> Zn分别为0.11至0.31‰，分别为0.33至0.42。大量不平衡局部Zn同位素分馏在Fe富含富含的橄榄石和曲氧酯中发生，具有δ 66 </ sup> Zn <sub> Opx-Ol </ sub>Δ=Δ0.50‰，Δ 66 </ sup> zn <sub> grt-ol </ sub>？= ?? 0.55至Δ0.39‰，Δ 66 </ sup> zn <sub> grt-opx </ sub>？= ?? 0.28到？ 0.05‰，δ 66 </ sup> zn <sub> grt-cpx </ sub>？= ?? 0.50至0.12‰。结合它们的低SiO <亚> 2 </ sub>含量和辐射性SR-ND-OS同位素组合物，Fe富含橄榄岩的高δ 66 </ sup> Zn归因于Mg-Lorzolites之间的反应并渗透SiO <sub> 2 </ sub>饱和玄武岩熔体，其掺入同位素重的地壳组分。通过岩石罩迁移的同位素重的渗透熔体的结晶产生高δ 66 </ sup> Zn Pyroxenites。曲克酸盐和大中际Zn同位素不平衡的低δ 66 </ sup> Zn可能由动力学Zn产生 </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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共17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=Huang Jian&option=202" target="_blank" rel="nofollow">Huang Jian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ackerman Luká?&option=202" target="_blank" rel="nofollow">Ackerman Luká?;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Xing‐Chao&option=202" target="_blank" rel="nofollow">Zhang Xing‐Chao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Fang&option=202" target="_blank" rel="nofollow">Huang Fang;</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>CAS Key Laboratory of Crust‐Mantle Materials and Environments School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Institute of Geology of the Czech Academy of SciencesPrague Czech Republic;</p> <p>CAS Key Laboratory of Crust‐Mantle Materials and Environments School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>CAS Key Laboratory of Crust‐Mantle Materials and Environments School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</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=zinc isotopes&option=203" rel="nofollow">zinc isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=peridotite&option=203" rel="nofollow">peridotite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pyroxenite&option=203" rel="nofollow">pyroxenite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=melt‐rock reaction&option=203" rel="nofollow">melt‐rock reaction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle heterogeneity&option=203" rel="nofollow">mantle heterogeneity;</a> </p> <div class="translation"> 机译：锌同位素;恒星;辉兴;熔岩反应;披风异质性; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591739.html">Mantle Zn Isotopic Heterogeneity Caused by Melt‐Rock Reaction: Evidence From Fe‐Rich Peridotites and Pyroxenites From the Bohemian Massif, Central Europe</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Jian&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Huang Jian,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ackerman Luká?&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ackerman Luká?,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Xing‐Chao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Xing‐Chao,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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