Three‐dimensional texture of natural pseudotachylyte: Pseudotachylyte formation mechanism in hydrous accretionary complex

Hamada Yohei; Kimura Gaku; Kameda Jun; Yamaguchi Asuka; Hamahashi Mari; Fukuchi Rina; Kitamura Yujin; Okamoto Shinya

摘要

Abstract > Melt‐origin pseudotachylyte is the most reliable seismogenic fault rock. It is commonly believed that pseudotachylyte generation is rare in the plate subduction zone where interstitial fluids are abundant and can trigger dynamic fault‐weakening mechanisms such as thermal pressurization. Some recent studies, however, have discovered pseudotachylyte‐bearing faults in exhumed ancient accretionary complexes, indicating that frictional melting also occurrs during earthquakes in subduction zones. To clarify the pseudotachylyte generation mechanism and the variation of slip behavior in the plate subduction zone, a pseudotachylyte found in the exhumed fossil accretionary complex (the Shimanto Belt, Nobeoka, Japan) was re‐focused and microscopic and three‐dimensional observations of the pseudotachylyte‐bearing fault were performed based on optical, electron, and X‐ray microscope images. Based on the patterns contained in the fragment, the pseudotachylyte is divided into four domains, although no clear domain boundaries or layering structures are not found. Three‐dimensional observation also suggests that the pseudotachylyte were fragmented or isolated by cataclasite or carbonate breccia. The pseudotachylyte was rather injected into the surrounding carbonate breccia, which is composed of angular fragments of the host rock and a matrix of tiny crystalline carbonate. The pseudotachylyte volume was extracted from the X‐ray microscope image and the heat abundance consumed by the pseudotachylyte generation was estimated at 2.18 MJ/m 2 , which can be supplied during a slip of approximately 0.5 m. These observations and calculations, together with the results of the previous investigations, suggest hydrofracturing and rapid carbonate precipitation that preceded or accompanied the frictional melting. Dynamic hydrofracturing during a slip can be ca </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”>摘录</ title> >熔体原点pseudotachyte是最可靠的地源性断裂岩。通常认为，在间质液体丰富的板俯口区域中，假壳体产生罕见，并且可以引发动态断层弱化机制，例如热压力。然而，最近的一些研究发现了膨胀的古老累积复合物中的假壳含有含量的缺陷，表明摩擦熔化也发生在俯冲区域的地震期间。为了阐明假咬的生成机制和板俯冲区中的滑移行为的变化，在挖掘化石增生复合体（Shimanto Belt，Nobeoka，日本）中发现的假辐射裂解物被重新聚焦和微观和三维观察伪沉积物 - 基于光学，电子和X射线显微镜图像进行 - 承包故障。基于片段中含有的图案，假奇晶特地被分成四个域，尽管未找到清晰的畴边界或分层结构。三维观察还表明假辐射裂解物被裂解或分离的碳酸酯或碳酸盐Breccia分离或分离。将假静脉注射到周围的碳酸盐Breccia中，该Breccia由宿主岩的角碎片和微晶碳酸酯的基质组成。从X射线显微镜图像中提取假壳晶体体积，并估计由假咬合生成消耗的热丰度为2.18mJ / m 2 </ sup>，其可以在约0.5米的滑动期间供应。这些观察和计算以及先前调查的结果表明，在摩擦熔化之前或伴随的碳酸氢脱水和快速的碳酸沉淀。滑动期间的动态水压性能可以是CA </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-30952/'>《The island arc》</a> <b style="margin: 0 2px;">|</b><span>2018年第2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=Hamada Yohei&option=202" target="_blank" rel="nofollow">Hamada Yohei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kimura Gaku&option=202" target="_blank" rel="nofollow">Kimura Gaku;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kameda Jun&option=202" target="_blank" rel="nofollow">Kameda Jun;</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=Hamahashi Mari&option=202" target="_blank" rel="nofollow">Hamahashi Mari;</a> <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=Kitamura Yujin&option=202" target="_blank" rel="nofollow">Kitamura Yujin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Okamoto Shinya&option=202" target="_blank" rel="nofollow">Okamoto Shinya;</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>Kochi Institute for Core Sample ResearchJapan Agency for Marine‐Earth Science and Technology 200 Monobe OtsuNankoku‐city Kochi 783‐8502 Japan;</p> <p>Office of Liaison and Cooperative ResearchTokyo University of Marine Science and Technology 4‐5‐7 Konan Minato–kuTokyo 108–8477 Japan;</p> <p>Department of Natural History Sciences Graduate School of ScienceHokkaido University N10‐W8 Kita‐kuSapporo‐shi Hokkaido 060‐0808 Japan;</p> <p>Atmosphere and Ocean Research InstituteThe University of Tokyo 5‐1‐5 KashiwanohaKashiwa‐shi Chiba 277‐8564 Japan;</p> <p>Office of Liaison and Cooperative ResearchTokyo University of Marine Science and Technology 4‐5‐7 Konan Minato–kuTokyo 108–8477 Japan;</p> <p>Atmosphere and Ocean Research InstituteThe University of Tokyo 5‐1‐5 KashiwanohaKashiwa‐shi Chiba 277‐8564 Japan;</p> <p>Department of Earth and Environmental SciencesGraduate School of Science and Engineering Kagoshima University 1‐21‐35 KorimotoKagoshima 890‐0065 Japan;</p> <p>Office of Liaison and Cooperative ResearchTokyo University of Marine Science and Technology 4‐5‐7 Konan Minato–kuTokyo 108–8477 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>P313.7; </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=fault dynamic lubrication&option=203" rel="nofollow">fault dynamic lubrication;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydrofracturing&option=203" rel="nofollow">hydrofracturing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=micro X‐ray CT&option=203" rel="nofollow">micro X‐ray CT;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nobeoka Thrust&option=203" rel="nofollow">Nobeoka Thrust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=plate subduction zone&option=203" rel="nofollow">plate subduction zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pseudotachylyte&option=203" rel="nofollow">pseudotachylyte;</a> </p> <div class="translation"> 机译：故障动态润滑;水力安全性;微X射线CT;Nobeoka推力;板俯冲区;假奇; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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/0704024846970.html">Three‐dimensional texture of natural pseudotachylyte: Pseudotachylyte formation mechanism in hydrous accretionary complex</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hamada Yohei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hamada Yohei,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kimura Gaku&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kimura Gaku,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kameda Jun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kameda Jun,</a> <a href="/journal-foreign-30952/" target="_blank" rel="nofollow" class="tuijian_authcolor">The island arc .</a> <span>2018</span><span>,第2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：天然假壳的三维纹理：含水增冲性络合物中的假囊形成机制</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_journal-structural-geology_thesis/0204112255882.html">Pseudotachylytes in an ancient accretionary complex and implications for melt lubrication during subduction zone earthquakes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kohtaro Ujiie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kohtaro Ujiie,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haruka Yamaguchi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Haruka Yamaguchi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arito Sakaguchi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Arito Sakaguchi,</a> <a href="/journal-foreign-851/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of structural geology .</a> <span>2007</span><span>,第4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：古代增生复合物中的拟速溶电解质及其在俯冲带地震中对熔体润滑的影响</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_detail_thesis/0204116711470.html">Dynamics of Earthquake Faulting in Subduction Zones: Inference from Pseudotachylytes and Ultracataclasites in an Ancient Accretionary Complex</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=K.Ujiie&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">K.Ujiie </a> <a href="/journal-foreign-27928/" target="_blank" rel="nofollow" class="tuijian_authcolor">Scientific Drilling .</a> <span>2007</span><span>,第SpecialIssue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：俯冲带地震断层的动力学：来自古增生复合体中的假速溶和超催化分解的推论</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_meeting-250680_thesis/070508668754.html">EXAFS ANALYSES OF INNERSPHERE COMPLEXATIONS OF ARSENATE AND SILICATE ON NATURAL HYDROUS FERRIC OXIDES</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Caterina E. 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