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Paleothermal structure of the NN ankai inner accretionary wedge estimated from vitrinite reflectance of cuttings

机译:苍白的结构 n n Ankai内部吸收楔估计从嵌管的vitriinite反射

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摘要

Abstract >The paleothermal structure and tectonic evolution of an accretionary prism is basic information for understanding subduction zone seismogenesis. To evaluate the entire paleotemperature profile of the Integrated Ocean Drilling Program (IODP) Site C0002 located in the off‐Kumano region of the Nankai Trough and penetrate the inner accretionary wedge down to 3058.5 m below the seafloor (mbsf), we performed a vitrinite reflectance analysis for cuttings and core samples during IODP expeditions 338 and 348: Nankai Trough seismogenic zone experiment. Although vitrinite reflectance values (Ro) tend to increase with depth, two reversals of these values suggested the existence of thrust fault zones with sufficient displacements to offset the paleothermal structure. The estimated maximum paleotemperatures are 42–70°C at 1200–1300 mbsf, 44–100°C at 1600–2400 mbsf, and 56–115°C at 2600–3000 mbsf, respectively. These temperatures roughly coincide with estimated modern temperatures; however, at a smaller scale, the reconstructed partial paleogeothermal gradient (~60–150°C/km) recorded at the hanging‐ and footwall of the presumed thrust fault zone is higher than the modern geothermal gradient (~30–40°C/km). This high paleogeothermal gradient was possibly obtained prior to subduction, reflecting the large heat flow of the young Philippine Sea Plate. </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> >苍白棱镜的苍白结构和构造演进是理解潜水区中生的基本信息。为了评估位于Nankai槽的羽绒地区的综合海洋钻井计划(IODP)站点C0002的整个古温度剖面,并穿过海底(MBSF)下方的内部增压楔下来至3058.5米,我们进行了vitriinite反射率IODP探险期间的切屑和核心样本分析338和348:Nankai Trough Seismogensic区实验。虽然Vitriinite反射率值(RO)随着深度倾向于增加,但是这些值的两个逆转表明,具有足够的位移的推力断层区的存在以抵消苍白的结构。估计的最大古葡萄球菌为42-70°C,为1200-1300 MBSF,44-100°C为1600-2400 MBSF,分别为56-115°C,为2600-3000 MBSF。这些温度大致重合,估计现代温度;但是,在较小的规模中,在假定的推力断裂带的悬挂和脚壁上录制的重建部分热坡梯度(〜60-150°C / km)高于现代地热梯度(〜30-40°C / km)。这种高古地热梯度可能在俯冲之前获得,反映了年轻菲律宾海底的大热流。</ 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8期</span><b style="margin: 0 2px;">|</b><span>共12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=Fukuchi Rina&option=202" target="_blank" rel="nofollow">Fukuchi Rina;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamaguchi Asuka&option=202" target="_blank" rel="nofollow">Yamaguchi Asuka;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yamamoto Yuzuru&option=202" target="_blank" rel="nofollow">Yamamoto Yuzuru;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ashi Juichiro&option=202" target="_blank" rel="nofollow">Ashi Juichiro;</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>Atmosphere and Ocean Research Institute University of TokyoKashiwa Japan;</p> <p>Atmosphere and Ocean Research Institute University of TokyoKashiwa Japan;</p> <p>Department of Mathematical Science and Advanced TechnologyJapan Agency for Marine‐Earth Science and TechnologyYokohama Japan;</p> <p>Atmosphere and Ocean Research Institute University of TokyoKashiwa 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=vitrinite reflectance&option=203" rel="nofollow">vitrinite reflectance;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nankai accretionary prism&option=203" rel="nofollow">Nankai accretionary prism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=cuttings&option=203" rel="nofollow">cuttings;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=IODP&option=203" rel="nofollow">IODP;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=inner wedge&option=203" rel="nofollow">inner wedge;</a> </p> <div class="translation"> 机译:vitriinite反射率;南开accreetionary棱镜;扦插;iodp;内楔; 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高敬鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,高敬鹏</a> <span> <a href="/journal-cn-5218/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 应用科技 </a> </span> <span> . 2021</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_petroleum-processing-petrochemicals_thesis/0201218184139.html">FCC进料雾化喷嘴结构对内部流场及混合特性的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李欣疏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李欣疏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘雪东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘雪东</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李柏贤&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李柏贤</a> <span> <a 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