Generation of Silicic Melts in the Early Izu‐Bonin Arc Recorded by Detrital Zircons in Proximal Arc Volcaniclastic Rocks From the Philippine Sea

Barth A. P.; Tani K.; Meffre S.; Wooden J. L.; Coble M. A.; Arculus R. J.; Ishizuka O.; Shukle J. T.

摘要

Abstract >A 1.2 km thick Paleogene volcaniclastic section at International Ocean Discovery Program Site 351‐U1438 preserves the deep‐marine, proximal record of Izu‐Bonin oceanic arc initiation, and volcano evolution along the Kyushu‐Palau Ridge (KPR). Pb/U ages and trace element compositions of zircons recovered from volcaniclastic sandstones preserve a remarkable temporal record of juvenile island arc evolution. Pb/U ages ranging from 43 to 27 Ma are compatible with provenance in one or more active arc edifices of the northern KPR. The abundances of selected trace elements with high concentrations provide insight into the genesis of U1438 detrital zircon host melts, and represent useful indicators of both short and long‐term variations in melt compositions in arc settings. The Site U1438 zircons span the compositional range between zircons from mid‐ocean ridge gabbros and zircons from relatively enriched continental arcs, as predicted for melts in a primitive oceanic arc setting derived from a highly depleted mantle source. Melt zircon saturation temperatures and Ti‐in‐zircon thermometry suggest a provenance in relatively cool and silicic melts that evolved toward more Th and U‐rich compositions with time. Th, U, and light rare earth element enrichments beginning about 35 Ma are consistent with detrital zircons recording development of regional arc asymmetry and selective trace element‐enriched rear arc silicic melts as the juvenile Izu‐Bonin arc evolved. </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> >在国际海洋发现计划网站351-u1438厚古古代火山体系351-u1438保留了深海海洋，近端的伊豆 - 波林海洋弧启动，沿着九州 - 帕劳山脊（KPR）的火山进化。从火山砂岩中回收的锆石和痕量元素组合物，保持了少年岛弧进化的显着时间记录。从43到27 ma的Pb / u老年都与北方Kpr北部的一个或多个活跃弧辅物中的出差相容。具有高浓度的所选微量元素的丰度提供了对U1438 Detrital锆石宿主熔体的成因的洞察力，并且代表了电弧环境中熔体组合物的短期和长期变化的有用指标。该网站U1438 Zircons跨越来自相对富集的大陆弧的中海脊Gabbros和锆锆的锆石之间的组成范围，这预测来自源自高耗尽的地幔源的原始海洋电弧环境中的熔体。熔融锆石饱和温度和Ti-In-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-in-silicic熔体的出处，其朝向更多的时间和富含富含的组合物。 Th，U和光稀土元素浓缩从大约35 mA开始，符合淡化锆石的替代Zircons记录区域弧不对称和选择性痕量元素的后弧硅熔体作为少年Izu-bonin弧的演变。</ 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10期</span><b style="margin: 0 2px;">|</b><span>共16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=Barth A. P.&option=202" target="_blank" rel="nofollow">Barth A. P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tani K.&option=202" target="_blank" rel="nofollow">Tani K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meffre S.&option=202" target="_blank" rel="nofollow">Meffre S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wooden J. L.&option=202" target="_blank" rel="nofollow">Wooden J. L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Coble M. A.&option=202" target="_blank" rel="nofollow">Coble M. A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arculus R. J.&option=202" target="_blank" rel="nofollow">Arculus R. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ishizuka O.&option=202" target="_blank" rel="nofollow">Ishizuka O.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shukle J. T.&option=202" target="_blank" rel="nofollow">Shukle J. T.;</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>Department of Earth SciencesIndiana University–Purdue University IndianapolisIndianapolis IN USA;</p> <p>Department of Geology and PaleontologyNational Museum of Nature and ScienceTsukuba Japan;</p> <p>CODES ARC Centre of Excellence in Ore DepositsUniversity of TasmaniaHobart TAS Australia;</p> <p>Retired from U.S. Geological SurveyMenlo Park CA USA;</p> <p>Department of Geological SciencesStanford UniversityStanford CA USA;</p> <p>Research School of Earth SciencesAustralian National UniversityActon Canberra ACT Australia;</p> <p>Geological Survey of Japan/AISTTsukuba Japan;</p> <p>Department of Earth SciencesIndiana University–Purdue University IndianapolisIndianapolis IN 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=detrital ziron&option=203" rel="nofollow">detrital ziron;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=submarine arc&option=203" rel="nofollow">submarine arc;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geochronology&option=203" rel="nofollow">geochronology;</a> </p> <div class="translation"> 机译：滴乳Ziron;潜艇弧;地理学论; </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/0704023360580.html">Generation of Silicic Melts in the Early Izu‐Bonin Arc Recorded by Detrital Zircons in Proximal Arc Volcaniclastic Rocks From the Philippine Sea</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barth A. 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href="/patent-detail/06120661151.html">从氧化钇稳定氧化锆固熔体废物中回收氧化锆及氧化钇的方法</a> <b>[P]</b> . <span> 中国专利： CN101244843B </span> <span> . 2010.08.18</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120105444587.html">从氧化钇稳定氧化锆固熔体废物中回收氧化锆及氧化钇的方法</a> <b>[P]</b> . <span> 中国专利： CN101244843A </span> <span> . 2008-08-20</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130417748695.html">Method for providing a search of interest group, media present storage that can be read by computer search system of information to provide the search of information to provide the search of the interest group executed by human searchers, media present storage that can be read For the computer to control to control a computer that includes a record of interest group.Media present storage that can be read by computer to control a computer that includes a record of the searcher of the interest group, media present storage that can be read 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