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Metamorphic olivine after dehydration embrittlement in Serpentinite: Case study from the Shiraga Serpentinite mass in the Sanbagawa high P/T metamorphic belt, central Shikoku, Japan

机译：蛇肽脱水脆化后的变质橄榄石：Sanbagawa高p / T变形带，中央Shikoku，Shiraga Serpentinite Mass的案例研究

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Abstract >Metamorphic olivine veins in serpentinites are considered to be a metamorphism dehydration product. However, the previous descriptions of these veins have been from paleo‐collision belts such as those in the Alps, Norwegian Caledonides, and Spain. Here the unique metamorphic olivine veins in a mass of serpentinite in the high‐pressure/low‐temperature (high P/T) Sanbagawa belt was reported. The Sanbagawa belt is a product of the subduction of oceanic plates during the Cretaceous. Elongated olivine‐talc veins were observed along shear bands in serpentine mylonite. The olivine's chemical composition is nearly pure forsterite; magnetite is distributed along the boundary of the olivine vein. This clearly suggests that the olivine was formed by the antigorite terminal reaction at a pressure less than 1.5?GPa. The reaction was caused by local heating in the mylonite as there is little evidence of the continuous antigorite breakdown reaction in the serpentinite. Metamorphic olivines are possibly formed in the intraslab earthquake zone of a relatively warm subduction zone such as southwest Japan after the antigorite terminal reaction at P less than 1.5?GPa. </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”XML：Lang =“en”> <标题类型=“main”>蛇形素中的变质橄榄石静脉被认为是变质脱水产品。然而，以前的这些静脉描述了来自古碰撞的皮带，例如阿尔卑斯山，挪威院和西班牙。这里报道了在高压/低温（高P / T）Sanbagawa带上质量蛇形素的独特变质橄榄石静脉。 Sanbagawa皮带是白垩纪期间海洋板俯冲的产物。沿蛇氨铁矿中的剪切带观察着细长的橄榄石滑石静脉。橄榄石的化学成分几乎是纯粹的插入物;磁铁矿沿橄榄石静脉的边界分布。这清楚地表明橄榄石由抗原型末端反应形成小于1.5μm≤GPA的压力。反应是由氨基钛矿中的局部加热引起的，因为六萜镁中连续的防雷氏菌分解反应很少有证据。变质橄榄石可能在intrAllab的intrallab地震区中形成在相对温暖的俯冲区，例如西南日本在少于1.5μm的末端反应后，如1.5μl。</ 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-30952/'>《The island arc》</a> <b style="margin: 0 2px;">|</b><span>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共10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=Fukumura Seiya&option=202" target="_blank" rel="nofollow">Fukumura Seiya;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Okamoto Kazuaki&option=202" target="_blank" rel="nofollow">Okamoto Kazuaki;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Terabayashi Masaru&option=202" target="_blank" rel="nofollow">Terabayashi Masaru;</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>Faculty of EducationSaitama University Shimo‐Okubo 255Saitama 338‐8570 Japan;</p> <p>Faculty of EducationSaitama University Shimo‐Okubo 255Saitama 338‐8570 Japan;</p> <p>Faculty of Engineering and DesignKagawa UniversityTakamatsu 761‐0396 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=dehydration embrittlement&option=203" rel="nofollow">dehydration embrittlement;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=metamorphic olivine in shear bands&option=203" rel="nofollow">metamorphic olivine in shear bands;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=origin of slab earthquake&option=203" rel="nofollow">origin of slab earthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=serpentinite in high P/T metamorphic belt&option=203" rel="nofollow">serpentinite in high P/T metamorphic belt;</a> </p> <div class="translation"> 机译：脱水脆化;剪切带中的变质橄榄石;板坯地震起源;高p / t变形带的蛇形岩; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024846895.html">Comment on 'Metamorphic olivine after dehydration embrittlement in Serpentinite: Case study from the Shiraga Serpentinite mass in the Sanbagawa high P/T metamorphic belt, central Shikoku, Japan' by Fukumura, Okamoto and Terabayashi, https://doi.org/10.1111/iar.12293</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wallis Simon R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wallis Simon R.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Endo Shunsuke&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Endo Shunsuke </a> <a href="/journal-foreign-30952/" target="_blank" rel="nofollow" class="tuijian_authcolor">The island arc .</a> <span>2020</span><span>,第1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：塞尾岩脱水脆化后的“变质橄榄石”：Sanbagawa High P / T变形带，中央Shikoku，日本的Shiraga Serpentinite Mass，HTTPS://Doi.org/10.11111/111111/ IAR.12293.</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070405080328.html">EBSD-measured crystal preferred orientation of eclogites from the Sanbagawa metamorphic belt, central Shikoku, SW Japan</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rehman Hafiz Ur&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Rehman Hafiz Ur,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mainprice David&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mainprice David,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barou Fabrice&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Barou Fabrice,</a> <a href="/journal-foreign-22881/" target="_blank" rel="nofollow" class="tuijian_authcolor">European journal of mineralogy .</a> <span>2016</span><span>,第6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：EBSD测量的日本四国中部Sanbagawa变质带中榴辉岩的晶体优选取向</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070408161523.html">Comment on 'Metamorphic P-T-time history of the Sanbagawa belt in central Shikoku, Japan and implications for retrograde metamorphism during exhumation' by K. Aoki, K. Kitajima, H. Masago, M. Nishizawa, M. Terabayashi, S. Omori, T. Yokoyama, N. Takahata, Y. Sano, S. Maruyama [Lithos 113 (2009) 393-407]</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S.R. Wallis&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">S.R. Wallis,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S. Endo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">S. 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tuijian_authcolor">Kazuaki Okamoto,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Masaru Terabayashi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Masaru Terabayashi </a> <span>2020</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：回复对蛇形素脱水脆化后的“变质橄榄石”的回答：Sanbagawa High P / T变形传染性的Shiraga Serpentinite Mass，Wallis和Endo，HTTPS://doi.org/10.111111/111111/111111/ IAR.12328.</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: 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