Tuffaceous Mud is a Volumetrically Important Volcaniclastic Facies of Submarine Arc Volcanism and Record of Climate Change

Gill J. B.; Bongiolo E. M.; Miyazaki T.; Hamelin C.; Jutzeler M.; DeBari S.; Jonas A‐S.; Vaglarov B. S.; Nascimento L. S.; Yakavonis M.

摘要

Abstract >The inorganic portion of tuffaceous mud and mudstone in an oceanic island arc can be mostly volcanic in origin. Consequently, a large volume of submarine volcaniclastic material is as extremely fine‐grained as products of subaerial eruptions (100 μm). Using results of IODP Expedition 350 in the Izu rear arc, we show that such material can accumulate at high rates (12–20 cm/k.y.) within 13 km of the nearest seamount summit and scores of km behind the volcanic front. The geochemistry of bulk, acid‐leached mud, and its discrete vitriclasts, shows that 75% of the mud is volcanic, and that most of it was derived from proximal rear arc volcanic sources. It faithfully preserves integrated igneous geochemical information about arc evolution in much the same way that terrigenous shales track the evolution of continental crust. In addition, their high sedimentation rate enables high resolution study of climate cycles, including the effects of Pleistocene glaciation on the behavior of the Kuroshio Current in the Shikoku Basin south of Japan. </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> >海洋岛弧中的臭泥浆和泥岩的无机部分主要是原产地的火山。因此，大量的潜水管血管基体材料如脱粒爆发的产物（＆100μm）。使用IZU后弧中IODP探险350的结果，我们表明这种材料可以高速累积（12-20cm / K.y。散装的地球化学，酸浸泥土及其离散的脱盐剂，表明了＆ 75％的泥浆是火山，并且其大部分来自近端后弧火山源。它忠实地保留了有关弧形演变的集成导致地球化学信息，同时是人造罗斯追踪大陆地壳的演变。此外，它们的高沉降率能够实现气候循环的高分辨率研究，包括百良生物冰川对日本Shikoku盆地的Kuroshio电流行为的影响。</ 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4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=Gill J. B.&option=202" target="_blank" rel="nofollow">Gill J. B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bongiolo E. M.&option=202" target="_blank" rel="nofollow">Bongiolo E. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Miyazaki T.&option=202" target="_blank" rel="nofollow">Miyazaki T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hamelin C.&option=202" target="_blank" rel="nofollow">Hamelin C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jutzeler M.&option=202" target="_blank" rel="nofollow">Jutzeler M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=DeBari S.&option=202" target="_blank" rel="nofollow">DeBari S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jonas A‐S.&option=202" target="_blank" rel="nofollow">Jonas A‐S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vaglarov B. S.&option=202" target="_blank" rel="nofollow">Vaglarov B. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nascimento L. S.&option=202" target="_blank" rel="nofollow">Nascimento L. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yakavonis M.&option=202" target="_blank" rel="nofollow">Yakavonis M.;</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 and Planetary SciencesUniversity of California Santa CruzSanta Cruz CA USA;</p> <p>Departamento de GeologiaUniversidade Federal do Rio de JaneiroRio de Janeiro Brazil;</p> <p>Department of Solid Earth GeochemistryJapan Agency for Marine‐Earth Science and TechnologyYokosuka Japan;</p> <p>K.G. Jebsen Centre for Deep Sea Research Department of Earth ScienceUniversity of BergenBergen Norway;</p> <p>School of Natural Sciences and CODES ‐ Centre for Ore Deposit and Earth SciencesUniversity of TasmaniaHobart TAS Australia;</p> <p>Geology DepartmentWestern Washington UniversityBellingham WA USA;</p> <p>Institut für GeowissenschaftenUniversity of KielKiel Germany;</p> <p>Department of Solid Earth GeochemistryJapan Agency for Marine‐Earth Science and TechnologyYokosuka Japan;</p> <p>Departamento de GeologiaUniversidade Federal do Rio de JaneiroRio de Janeiro Brazil;</p> <p>Geology DepartmentWestern Washington UniversityBellingham WA 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=volcanism&option=203" rel="nofollow">volcanism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcaniclastic sediment&option=203" rel="nofollow">volcaniclastic sediment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment geochemistry&option=203" rel="nofollow">sediment geochemistry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=island arc&option=203" rel="nofollow">island arc;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kuroshio current&option=203" rel="nofollow">Kuroshio current;</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> </p> <div class="translation"> 机译：山脉;火山岩沉积物;沉积地球化学;岛弧;Kuroshio Current;IoDP; </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/0704023360309.html">Tuffaceous Mud is a Volumetrically Important Volcaniclastic Facies of Submarine Arc Volcanism and Record of Climate Change</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gill J. 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