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Magmatic Response to Subduction Initiation: Part 1. Fore‐arc Basalts of the Izu‐Bonin Arc From IODP Expedition 352

机译：对郊区启动的岩浆反应：第1部分。来自IODP探险的Izu-Bonin弧的前弧底座352

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Abstract > The Izu‐Bonin‐Mariana (IBM) fore arc preserves igneous rock assemblages that formed during subduction initiation circa 52?Ma. International Ocean Discovery Program (IODP) Expedition 352 cored four sites in the fore arc near the Ogasawara Plateau in order to document the magmatic response to subduction initiation and the physical, petrologic, and chemical stratigraphy of a nascent subduction zone. Two of these sites (U1440 and U1441) are underlain by fore‐arc basalt (FAB). FABs have mid‐ocean ridge basalt (MORB)‐like compositions, however, FAB are consistently lower in the high‐field strength elements (TiO <sub>2</sub> , P <sub>2</sub> O <sub>5</sub> , Zr) and Ni compared to MORB, with Na <sub>2</sub> O at the low end of the MORB field and FeO* at the high end. Almost all FABs are light rare earth element depleted, with low total REE, and have low ratios of highly incompatible to less incompatible elements (Ti/V, Zr/Y, Ce/Yb, and Zr/Sm) relative to MORB. Chemostratigraphic trends in Hole U1440B are consistent with the uppermost lavas forming off axis, whereas the lower lavas formed beneath a spreading center axis. Axial magma of U1440B becomes more fractionated upsection; overlying off‐axis magmas return to more primitive compositions. Melt models require a two‐stage process, with early garnet field melts extracted prior to later spinel field melts, with up to 23% melting to form the most depleted compositions. Mantle equilibration temperatures are higher than normal MORB (1,400?°C–1,480?°C) at relatively low pressures (1–2?GPa), which may reflect an influence of the Manus plume during subduction initiation. Our data support previous models of FAB origin by decompression melting but imply a source more depleted than normal MORB source mantle. </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> > Izu-Bonin-Mariana（IBM）前电弧保留在俯冲开始期间形成的火成岩组合，这是第52型拍摄期间。国际海洋发现计划（IODP）探险队在ogasawara高原附近的前弧中的核心四个地点，以便将岩层响应和新生俯冲区的物理，岩画和化学层次作用。这些网站中的两个（U1440和U1441）是通过前弧玄武岩（Fab）的下层。 Fabs有中海脊玄武岩（Morb） - 麦克风组合物，然而，Fab在高场强元件中始终如一地低（TiO <sub> 2 </ sub> ，P. <sub> 2 </ sub> O. <sub> 5 </ sub> ，zr）和ni与morb相比，na <sub> 2 </ sub> o在Morb领域的低端和高端的Feo *。几乎所有Fab都是轻质稀土元素耗尽，总重量低，并且相对于Morb的较少不相容的元素（Ti / V，Zr / Y，Ce / Yb和Zr / Sm）具有低比率。孔U1440b的化学色点趋势与形成轴的最上层的熔岩符合，而下熔岩形成在扩散中心轴下。 U1440B的轴向岩浆变得更加分离;覆盖轴轴岩浆返回更多的原始组合物。熔融模型需要两级工艺，早期石榴石熔接在后来的尖晶石场熔化之前提取，熔化程度高达23％以形成最耗尽的组合物。在相对低的压力下（1-2μl≤GPA），地幔平衡温度高于正常的MARB（1,400？°C-1,480℃），这可能反映了在俯冲开始期间甘蓝羽的影响。我们的数据通过解压缩熔化支持以前的Fab Oigin的型号，但暗示比普通的Morb源地幔更耗尽。 </ 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1期</span><b style="margin: 0 2px;">|</b><span>共25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=Shervais John W.&option=202" target="_blank" rel="nofollow">Shervais John W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reagan Mark&option=202" target="_blank" rel="nofollow">Reagan Mark;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haugen Emily&option=202" target="_blank" rel="nofollow">Haugen Emily;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Almeev Renat R.&option=202" target="_blank" rel="nofollow">Almeev Renat R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pearce Julian A.&option=202" target="_blank" rel="nofollow">Pearce Julian A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Prytulak Julie&option=202" target="_blank" rel="nofollow">Prytulak Julie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ryan Jeffrey G.&option=202" target="_blank" rel="nofollow">Ryan Jeffrey G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Whattam Scott A.&option=202" target="_blank" rel="nofollow">Whattam Scott A.;</a> <a 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City IA USA;</p> <p>Department of GeologyUtah State UniversityLogan UT USA;</p> <p>Institut für MineralogieLeibniz Universit?t HannoverHannover Germany;</p> <p>School of Earth and Ocean SciencesCardiff UniversityCardiff UK;</p> <p>Department of Earth SciencesUniversity of DurhamDurham UK;</p> <p>School of GeosciencesUniversity of South FloridaTampa FL USA;</p> <p>Department of GeosciencesKing Fahd University of Petroleum and MineralsDhahran Saudi Arabia;</p> <p>Géosciences Montpellier CNRSUniversité de MontpellierMontpellier France;</p> <p>School of GeosciencesUniversity of SydneySydney New South Wales Australia;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Institute of Earth Sciences NAWI Graz GeocenterUniversity of GrazGraz Austria;</p> <p>Department of Physics Astronomy and GeosciencesTowson UniversityTowson MD USA;</p> <p>CEOASOregon State UniversityCorvallis OR USA;</p> <p>Institut für MineralogieUniversit?t zu K?lnK?ln Germany;</p> <p>Japan Agency for Marine‐Earth Science and TechnologyKochi Institute for Core Sample ResearchKochi Japan;</p> <p>Department of ScienceOsaka UniversityOsaka Japan;</p> <p>Chinese Academy of Geological ScienceInstitute of GeologyBeijing China;</p> <p>Department of GeologyCentenary CollegeShreveport LA 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=Forearc basalts&option=203" rel="nofollow">Forearc basalts;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction initiation&option=203" rel="nofollow">subduction initiation;</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=Izu‐Bonin forearc&option=203" rel="nofollow">Izu‐Bonin forearc;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Joides Resolution&option=203" rel="nofollow">Joides Resolution;</a> </p> <div class="translation"> 机译：Forearc BasaLts;俯冲开始;眼镜岩;Izu-Bonin Forearc;加入解决方案; </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 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href="/journal-cn-56825/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋地质与第四纪地质 </a> </span> <span> . 2014</span><span>,第1期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geologica-sinica_thesis/0201252701757.html">柴达木盆地北缘早奥陶世陆-弧碰撞及弧后前陆盆地——来自碎屑岩地球化学的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙娇鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 孙娇鹏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈世悦&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陈世悦</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=马寅生&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,马寅生</a> <span> <a href="/journal-cn-4885/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质学报 </a> </span> <span> . 2016</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_earth-science-frontiers_thesis/0201253147956.html">陆内“滞后”弧岩浆岩特征及其地质意义:来自西准噶尔乌尔禾北早二叠世岩浆作用的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李永军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李永军</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐倩&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,徐倩</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨高学&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,杨高学</a> <span> <a href="/journal-cn-4911/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地学前缘 </a> </span> <span> . 2016</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" 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<span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=段瑞涵&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 段瑞涵</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘超辉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘超辉</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=施建荣&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,施建荣</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2021</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-43375_thesis/020222796649.html">幕式弧岩浆作用与大陆地壳生长和演化：来自冈底斯弧白垩纪侵入岩的制约</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈龙&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈龙</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑永飞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑永飞</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵子福&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵子福</a> <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/020313323272.html">甲烷部分氧化制合成气旋风滑弧非热等离子体反应器设计技术研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许国锋&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 许国锋</a> <span> . 2013</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130438274728.html">Method of and apparatus for controlling the selection, initiation and execution of computer programs automatically and directly in response to the remote (or proximal) scan of special barcodes or other coded indicia, as by a publication reader scanning such a barcode therein to access on a viewable computer or TV screen or the like, supplemental pictorial and other material related to the publication and stored on an internet website that is automatically accessed by the computer in direct response to receiving the barcode scan signals from the reader, and without other human intervention</a> <b>[P]</b> . <span> 外国专利：  US2006124742A1 </span> <span> . 2006-06-15</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：用于响应于特殊条形码或其他编码标记的远程（或近端）扫描而自动且直接地控制计算机程序的选择，启动和执行的方法和装置，例如通过出版物读取器在其中扫描此类条形码以访问计算机上的条形码。可见的计算机或电视屏幕等，与出版物有关的补充图片和其他材料，并存储在互联网网站上，计算机直接响应接收到阅读器的条形码扫描信号而自动访问该互联网网站，而无需其他人工干预 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130432871375.html">Method of and apparatus for controlling the selection, initiation and execution of computer programs automatically and directly in response to the remote (or proximal) scan of special barcodes or other coded indicia, in direct response to receiving the barcode scan signals from the reader, and without other human intervention</a> <b>[P]</b> . <span> 外国专利：  US7314178B2 </span> <span> . 2008-01-01</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：响应于特殊条形码或其他编码标记的远程（或近端）扫描，直接响应于从读取器接收到条形码扫描信号而自动和直接地控制计算机程序的选择，启动和执行的方法和装置，以及无需其他人为干预 </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 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