Differentiation of a Hydrous Arc Magma Recorded in Melt Inclusions in Deep Crustal Cumulate Xenoliths from Ichinomegata Maar, NE Japan

Yanagida Y.; Nakamura M.; Yasuda A.; Kuritani T.; Nakagawa M.; Yoshida T.

摘要

Abstract > The Ichinomegata maar, located in the back‐arc side of the northeastern Japan arc, erupted calc‐alkaline andesitic magma with abundant deep‐crustal and mantle xenoliths at about 60–80 ka. We investigated the relationship between fractionated solids and differentiated silicic melts at middle to lower crust conditions through petrologic analyses of hornblende‐bearing cumulate xenoliths and melt inclusions. The Sr and Nd isotope compositions are similar to those of the host magmas, suggesting their cognate origin. The crystallization sequence is determined to be olivine, spinel → clinopyroxene → hornblende, magnetite → plagioclase → apatite, based on the observation of texture and solid solution compositions. Of the five types of xenolith studied, the leuco‐hornblende gabbro preserved interstitial glass and melt inclusions with a silica content (SiO <sub>2</sub> ) of 63.9–74.0 wt % and high water content (up to 8.1 wt %). Hornblende geobarometry indicates an equilibrium pressure of 0.39–0.64 GPa, which corresponds to a depth of 15–24 km. The delay of plagioclase crystallization due to high water content characterizes differentiation of the hydrous arc magma. We successfully constructed an internally consistent differentiation model of the corundum‐normative calc‐alkaline trend to the silicic melt inclusions, starting from primitive basalt via successive fractionation of a calculated wherlite and cumulate xenoliths. In middle to late stage differentiation, hornblende gabbros are the dominantly fractionated assemblages. Our results are consistent with published differentiation experiments of hydrous arc magmas and the lithology of the deep crust beneath the back arc of the NE Japan arc as estimated from seismic tomography. </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> > Ichinomegata Maar位于日本东北部的后弧弧，爆发的钙碱性岩浆爆发了钙碱性岩浆，大约60-80 ka大约60-80 ka。我们通过岩石分析累积Xenoliths和熔融夹杂物，研究了中间到下壳条件下的分馏固体和分化的硅熔体之间的关系。 Sr和Nd同位素组合物与宿主岩浆的组合物类似，表明其同源原产地。将结晶序列确定为橄榄石，尖晶石→Clinococe→Hortblende，磁铁矿→Plagioclase→磷灰石，基于纹理和固溶组合物的观察。在研究五种类型的Xenolith中，Leuco-Hornblende Gabbro保存了间质玻璃和用二氧化硅含量的熔体夹杂物（SiO <sub> 2 </ sub> ）63.9-74.0wt％和高水含量（高达8.1wt％）。 Hornblende地质测量法表明0.39-0.64GPa的平衡压力，其对应于15-24公里的深度。由于高含水含量引起的普发基酶结晶的延迟表征了湿弧岩浆的分化。我们成功地构建了核心规范性钙碱趋势的内部一致的分化模型，以硅熔体夹杂物从原始玄武岩开始，通过计算出的次胶质和抵抗Xenoliths。在中期阶段分化中，Hornblende Gabbros是占分级的组装。我们的结果与湿弧磁带的公开差异化实验一致，据据抗震断层扫描估计，Ne Japan弧下方的深色地壳的岩性。 </ 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>2018年第3期</span><b style="margin: 0 2px;">|</b><span>共27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=Yanagida Y.&option=202" target="_blank" rel="nofollow">Yanagida Y.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakamura M.&option=202" target="_blank" rel="nofollow">Nakamura M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yasuda A.&option=202" target="_blank" rel="nofollow">Yasuda A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kuritani T.&option=202" target="_blank" rel="nofollow">Kuritani T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakagawa M.&option=202" target="_blank" rel="nofollow">Nakagawa M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yoshida T.&option=202" target="_blank" rel="nofollow">Yoshida 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 Science Graduate School of ScienceTohoku UniversitySendai Japan;</p> <p>Department of Earth Science Graduate School of ScienceTohoku UniversitySendai Japan;</p> <p>Earthquake Research Institute University of TokyoTokyo Japan;</p> <p>Graduate School of ScienceHokkaido UniversitySapporo Japan;</p> <p>Graduate School of ScienceHokkaido UniversitySapporo Japan;</p> <p>Department of Earth Science Graduate School of ScienceTohoku UniversitySendai Japan;</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=hornblende fractionation&option=203" rel="nofollow">hornblende fractionation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lower crust&option=203" rel="nofollow">lower crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cumulate xenoliths&option=203" rel="nofollow">cumulate xenoliths;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=calc‐alkaline&option=203" rel="nofollow">calc‐alkaline;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=alumina saturation index&option=203" rel="nofollow">alumina saturation index;</a> </p> <div class="translation"> 机译：角质分馏;下壳;累积Xenoliths;钙碱性;氧化铝饱和度指数; </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/0704023360796.html">Differentiation of a Hydrous Arc Magma Recorded in Melt Inclusions in Deep Crustal Cumulate Xenoliths from Ichinomegata Maar, NE Japan</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yanagida Y.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yanagida Y.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakamura M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Nakamura M.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yasuda A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yasuda A.,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第3期</span> </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：在Ne Japan的Ichinomegata Maar中，熔融夹杂物中熔化夹杂物中记录的湿弧岩浆的差异化</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024750932.html">Reconstruction of the lithosphere-asthenosphere boundary zone beneath Ichinomegata maar, Northeast Japan, by geobarometry of spinel peridotite xenoliths</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sato Yuto&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sato Yuto,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ozawa Kazuhito&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ozawa Kazuhito </a> <a href="/journal-foreign-30500/" target="_blank" rel="nofollow" class="tuijian_authcolor">The American mineralogist .</a> <span>2019</span><span>,第9a10期</span> </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：作者：王莹，王莹，王莹，王莹，王莹，王莹，王莹，王莹，王莹，王莹，王莹，王莹，王莹，王孝娣</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704018502734.html">Experimentally derived high-pressure cumulates from hydrous arc magmas and consequences for the seismic velocity structure of lower arc crust</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Muntener O&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Muntener O,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ulmer P&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ulmer P </a> <a href="/journal-foreign-23539/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geophysical Research Letters .</a> <span>2006</span><span>,第21期</span> </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：从含水弧岩浆中实验得出的高压积聚及其对下弧壳地壳地震速度结构的影响</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_first-meeting-asia-current-research-fluid-inclusion_thesis/020511370120.html">Study on melt inclusions in calcite from crust-derived carbonatite vein in diorite and in feldspar from diorite xenolith within crust-derived carbonatite at contact zone of Daye iron deposit, Hubei Province</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bin Zhao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bin Zhao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jinsong Zhao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jinsong Zhao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jincao Wang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jincao Wang,</a> <a href="/conference-foreign-20151/" target="_blank" rel="nofollow" class="tuijian_authcolor">First Meeting Asia Current Research on Fluid Inclusion: Program with Abstracts .</a> <span>2006</span> </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：湖北省大冶铁矿床接触带壳碳酸盐岩脉中方解石，方解石碳酸盐岩中长石和长石</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061536188.html">GRANULITE FACIES XENOLITHS FROM KILBOURNE HOLE MAAR, NEW MEXICO AND THEIR BEARING ON DEEP CRUSTAL EVOLUTION.</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=PADOVANI, ELAINE LOUISE REEVES.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">PADOVANI, ELAINE LOUISE REEVES. </a> <span>1977</span> </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：来自新墨西哥州基尔本·孔马尔的花岗岩相XENOLITHS及其对深层地壳演化的影响。</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_detail_thesis/040004644434.html">Crustal CO2 contribution to subduction zone degassing recorded through calc-silicate xenoliths in arc lavas</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sean Whitley&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sean Whitley,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ralf Gertisser&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ralf Gertisser,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ralf Halama&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ralf Halama,</a> <span>-1</span> </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：弧形熔岩中钙硅酸盐异岩记录的地壳二氧化碳对俯冲带脱气的贡献</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100019065403.html">High-Mg adakitic rocks and their complementary cumulates formed by crystal fractionation of hydrous mafic magmas in a continental crustal magma chamber</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ma Qiang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ma Qiang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Yi-Gang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xu Yi-Gang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Jian-Ping&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zheng Jian-Ping,</a> <span>2016</span> </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：高镁基质岩及其在陆壳岩浆室内水合镁铁质岩浆晶体分馏形成的互补堆积物</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-central-south-university-science-technology_thesis/0201248335411.html">低碳低合金钢中CaO-Al2O3-SiO2-MgO系夹杂物熔化温度的控制</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵烁&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵烁</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王谦&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王谦</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=徐建飞&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,徐建飞</a> <span> <a href="/journal-cn-4543/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中南大学学报（自然科学版） </a> </span> <span> . 2013</span><span>,第008期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_modern-metallurgy-inner-mongolia_thesis/0201262381894.html">Fe-Al-Ti合金在熔融和凝固态中的夹杂物行为</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ShotaAmano日本&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . ShotaAmano日本</a> <span> <a href="/journal-cn-39433/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 现代冶金（内蒙古） </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_steel-translation-set_thesis/0201220925758.html">Ca-Mn-Si-Al-O-S系硫氧化物夹杂物的热力学模型与数据库及其在钢中夹杂物演变预测方面的应用</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rongxun Piao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . Rongxun Piao</a> <span> <a href="/journal-cn-8047/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 钢铁译文集 </a> </span> <span> . 2015</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_metallurgical-analysis_thesis/0201220517836.html">火花源光发射光谱法分析钢中夹杂物的研究进展——夹杂物成分和尺寸的现象学分析与计算</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Edmund Halász&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . Edmund Halász</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kaizhen Li&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Kaizhen Li</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jean-Luc Dorier&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Jean-Luc Dorier</a> <span> <a href="/journal-cn-8021/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 冶金分析 </a> </span> <span> . 2011</span><span>,第010期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_physical-chemical-testing-volume_thesis/0201267250057.html">钢中夹杂物的鉴定方法及其进展：第二讲夹杂物的岩相及X射线衍射鉴定方法</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李静媛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李静媛</a> <span> <a href="/journal-cn-50988/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 理化检验：物理分册 </a> </span> <span> . 1993</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-28716_thesis/020222061527.html">钢中夹杂物组分在电解液中参与化学反应的热力学讨论——阳极泥法分离提取钢中夹杂物方法评价的研究(1)</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李宏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李宏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=宁林新&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,宁林新</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李景捷&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李景捷</a> <span> <a href="/conference-cn-28716/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第二届冶金工程科学论坛 </a> <span> <span> . 2003</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020316303338.html">海洋环境下低合金钢中夹杂物与腐蚀行为的关联性研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王宇航&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 王宇航</a> <span> . 2021</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120108289116.html">一种控制熔融金属中夹杂物尺寸及数量的方法</a> <b>[P]</b> . <span> 中国专利： CN105779692A </span> <span> . 2016-07-20</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120102109186.html">一种熔融金属中夹杂物及气泡的去除和细化方法</a> <b>[P]</b> . <span> 中国专利： CN103436655A </span> <span> . 2013-12-11</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130466453872.html">JAPANESE ARCHIPELAGO REMODELING METHOD WITH SUPER-DEEP UNDERGROUND TUNNEL</a> <b>[P]</b> . <span> 外国专利：  JPH02225800A </span> <span> . 1990-09-07</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：超深地下隧道的日本群岛重塑方法 </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;" onclick="ywcd('0704023360796','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p class="current">目前支持订阅全部北京大学中文核心（2020）期刊目录。</p> <div style="display: flex;margin-top: 69px;justify-content: space-between;"> <div class="no-sub" onclick="$('.journalsub-pop-up').hide()">暂不订阅</div> <div class="other-sub" onclick="continueSub('from=pc-detail')">继续订阅其他期刊</div> </div> </div> </div> <div class="right_btn"> <ul> <li class="gouwuche">  </li> <li class="yijian"> <a href="javascript:void(0);" onclick="link_analysis('/mycenter/auth/complaint.html',this)" title="意见反馈">意见反馈</a> </li> <li class="top"> <a href="javascript:scrollTo(0,0);" title="回到顶部">回到顶部</a> </li> <li class="shouye"> <a href="/" title="首页">回到首页</a> </li> </ul> </div> <div class="xllindexfooter"> <div class="xllindexfootercenter"> <div class="xllindexfooterleft left" > <div class="xllindexfooterleftli"> <ul> <li><a href="/about.html" title="关于掌桥">关于掌桥</a></li> <li><a href="/help/helpmap.html" title="资源导航">资源导航</a></li> <li><a href="/help/helpguide.html" title="新手指南">新手指南</a></li> <li><a href="/help/helpcenter.html" title="常见问题">常见问题</a></li> <li><a href="/sitemap.html" title="网站地图">网站地图</a></li> <li><a href="/help/helpcenter.html?type=9" title="版权声明">版权声明</a></li> </ul> </div> <div class="xllindexfooterleft"> <p class="xllindexfooterlefteamil">客服邮箱：kefu@zhangqiaokeyan.com</p> <div class="xllindexfooterlefttcp"> <div class="xllindexfooterpoliceiimg"></div> <div class="xllindexfooterpoliceispan"> <span>京公网安备：11010802029741号 </span> <span>ICP备案号：<a href="https://beian.miit.gov.cn" rel="nofollow" target="_blank" title="ICP备案号">京ICP备15016152号-6</a></span> <span>六维联合信息科技 (北京) 有限公司©版权所有</span> </div> </div> </div> </div> <div class="xllindexfooterright left"> <ul> <li> <p style="font-weight: bold;">客服微信</p> <div></div> </li> <li> <p style="font-weight: bold;">服务号</p> <div></div> </li> </ul> </div> </div> </div> <span id="0704023360796down" data-source="7," data-out-id="wYjLqjzT7ooDGf8AEC0z9xBXsFveIQoViAVJv+uiPfDkQJLjs7zWcSjKIl7QHlyW," data-f-source-id="7" data-title="Differentiation of a Hydrous Arc Magma Recorded in Melt Inclusions in Deep Crustal Cumulate Xenoliths from Ichinomegata Maar, NE Japan" data-price="20" data-site-name="" data-transnum="24" style="display:none;"></span> <input type="hidden" value="4" id="sourcetype"> <input type="hidden" value="23285" id="journalid"> <input type="hidden" value="1" id="inyn_provide_service_level"> <input type="hidden" value="https://cdn.zhangqiaokeyan.com" id="imgcdn"> <input type="hidden" value="1" id="isdeatail"> <input type="hidden" value="" id="syyn_indexed_database"> <input type="hidden" value="" id="servicetype"> <input type="hidden" id="pagename" value="Differentiation of a Hydrous Arc Magma Recorded in Melt Inclusions in Deep Crustal Cumulate Xenoliths from Ichinomegata Maar, NE Japan"/> <input type="hidden" value="thesis_get_original" id="pageIdentification"> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery-1.12.4.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/lwlh_ajax.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zq.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery.cookie.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/top.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/newmail.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.7.8"></script> <script type="text/javascript" src="https://www.zhangqiaokeyan.com/statistics/static/pagecollection.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/tj.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/sse.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/pushbaidu.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/history.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/util/cookie.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.7.8"></script> </body> <script> $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); var inyn_provide_service_level = $("#inyn_provide_service_level").val(); if((sourcetype ==1||sourcetype==4)&&inyn_provide_service_level!=4){ getJournal(); } }) </script> </html>