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Preferential Orthopyroxene Serpentinization and Implications for Seismic Velocity Interpretation in the Fore‐Arc Mantle

机译：优先偏离术骨蛇形化及其对前弧地幔中地震速度解释的影响

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Abstract > For better interpretation of seismic tomography data of the hydrated fore‐arc mantle, we examined conditions of nonstoichiometric hydration of peridotite reported by a previous experimental study (i.e., preferential orthopyroxene (Opx) serpentinization and resultant talc formation) at 500–580?°C and under 0.8–1.8?GPa. The corresponding seismic velocity was calculated by considering the talc production. Talc formed under all the experimental conditions even in the olivine‐dominated system, in which the olivine to Opx ratio was 7:3 by weight. The amount of talc produced was comparable to that of serpentine at high temperature and low pressure and increased with increasing temperature and decreasing pressure due to decreasing contribution of olivine in the reaction. We also present a natural case of preferential Opx reaction in the Horoman peridotite complex, Japan, on the basis of its strong similarity in textures and mineral phases to our experimental products obtained at 0.8–1.3?GPa. Calculations on seismic velocities of hydrated harzburgite using the Voigt‐Reuss‐Hill averaging scheme showed that the formation of talc along with antigorite leads to a decrease in P wave ( V <sub>p</sub> ) and S wave velocities ( V <sub>s</sub> ) but no remarkable increase in V <sub>p</sub> / V <sub>s</sub> due to the lower V <sub>p</sub> / V <sub>s</sub> value of talc (~1.60) compared with that of antigorite (~1.77). Such a seismic anomaly has been observed in the shallow mantle wedge of the southern Western Alps subduction zone, where suppressed water supply from the subducted continental lithosphere might allow the persistenc </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”>抽象</ title> >，用于更好地解释水合前弧地幔的地震断层扫描数据，我们检查了条件通过先前的实验研究（即，优先偏异烯（OPX）蛇形化和合成的滑石形成）在500-580℃和0.8-1.8℃下进行恒星的非核心水合水合。通过考虑滑石制作来计算相应的地震速度。即使在橄榄石主导的体系中，所有实验条件下都在所有实验条件下形成的滑石，其中橄榄石到OPX比例为7：3重量。产生的滑石的量与高温低压下的蛇纹碱的量相当，随着橄榄胺贡献的贡献而增加，随着温度和降低的压力而增加。我们还在日本Horoman PeridoTite复合物中展示了优惠OPX反应的案例，其基于其在纹理和矿物阶段的强烈相似性，以在0.8-1.3〜3℃下获得的实验产物。使用Voigt-Reuss-Hill平均方案的水合哈尔茨堡的地震速度的计算表明，TALC与抗抗石的形成导致 P </ i>波（ v </ i> <sub）的降低> p </ sub>）和 s </ i>波速（ v </ i> <sub> s </ sub>），但没有显着增加 v </ i> <由于较低的 v </ i> <sub> p </ sub> / V </ i> <sub> s </ sum> v </ i> <sub> s </ sum>。 / i> <sub> s </ sub>滑石（〜1.60）的值与抗真的（〜1.77）相比。在南方西部阿尔卑斯山丘俯卧区的浅地幔楔形地区已经观察到这种地震异常，其中抑制了底层大陆岩石圈的供水可能允许持久化 </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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共16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=Nakatani T.&option=202" target="_blank" rel="nofollow">Nakatani T.;</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> </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> </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=serpentinization&option=203" rel="nofollow">serpentinization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=talc&option=203" rel="nofollow">talc;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=orthopyroxene&option=203" rel="nofollow">orthopyroxene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle wedge&option=203" rel="nofollow">mantle wedge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic velocity&option=203" rel="nofollow">seismic velocity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=piston cylinder&option=203" rel="nofollow">piston cylinder;</a> </p> <div class="translation"> 机译：蛇形化;滑石;矫形;地幔楔;地震速度;活塞缸; </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/0704025591017.html">Preferential Orthopyroxene Serpentinization and Implications for Seismic Velocity Interpretation in the Fore-Arc Mantle</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nakatani T.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Nakatani T.,</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="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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