Diffusion Creep of Enstatite at High Pressures Under Hydrous Conditions

机译：在含水条件下高压下山牙石的扩散蠕变

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Abstract > Mantle convection and large‐scale plate motion depend critically on the nature of the lithosphere‐asthenosphere boundary and thus on the viscosity structure of Earth's upper mantle, which is determined by the rheological properties of its constituent minerals. To constrain the flow behavior of orthopyroxene, the second most abundant constituent of the upper mantle, deformation experiments were carried out in triaxial compressive creep on fine‐grained (~6?μm) samples of enstatite at high pressures (3.8–6.3?GPa) and high temperatures (1323–1573?K) using a deformation‐DIA apparatus. Based on results from this study, the deformation behavior of enstatite is quantitatively presented in the form of a flow law that describes the dependence of deformation rate on differential stress, water fugacity, temperature, and pressure. Specifically, the creep rate depends approximately linearly on stress, indicating deformation in the diffusion creep regime. A least squares regression fit to our data yielded a flow law for diffusion creep with an activation energy of ~200?kJ/mol and an activation volume of ~14?×?10 ?6 ?m 3 /mol. The magnitude of the water‐weakening effect is similar to that for olivine with a water fugacity exponent of <fi>r</fi> ?≈?0.7. This strong dependence of viscosity on water fugacity (concentration) indicates that the viscosity of an orthopyroxene‐bearing mantle varies from one geological setting to another, depending on the large‐scale water distribution. Based on the rheology contrast between olivine and enstatite, we conclude that olivine is weaker than enstatite throughout most of the upper mantle except in some shallow regions in the diffusion creep regime. </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”>抽象</ title> >披风对流和大尺寸板运动依赖于岩石圈的性质 - 岩石圈的性质因此，通过其组成矿物质的流变性能决定的地地罩的粘度结构。为了限制正交性的流动行为，在高压下的细粒（〜6Ωμm）上的三轴压缩蠕变中，在高压下的微粒（〜6μm）样品上进行变形实验的第二个最丰富的成分。（3.8-6.3〜GPA）使用变形-DIA装置和高温（1323-1573 k）。基于本研究的结果，以流动规律的形式定量地呈现了尚尔特石的变形行为，所述流动法描述了变形率对差分应力，水逃逸度，温度和压力的依赖性。具体地，蠕变速率大致线性地对应力，表示扩散蠕变状态的变形。适合我们数据的最小二乘回归产生了一种流动法，用于扩散蠕变，其激活能量为〜200？kj / mol，激活体积为〜14Ω×10 Δ6</ sup>？m <sup > 3 </ sup> / mol。水弱效果的幅度与橄榄石的橄榄石的效果相似，具有<fi> R的水逃逸性指数</ fi>Δ0.7。这种强烈依赖于水逃逸度（浓度）表明，取决于大规模的水分布，轴承壳体的粘度从一个地质环境变化到另一个地质环境。基于Olivine和Enstatite之间的流变学对比，我们得出结论，除了在扩散蠕变状态下的一些浅地区之外，橄榄石在大多数上部地幔中较弱。 </ p> </ abstract> </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>2017年第10期</span><b style="margin: 0 2px;">|</b><span>共11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=Zhang Guinan&option=202" target="_blank" rel="nofollow">Zhang Guinan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mei Shenghua&option=202" target="_blank" rel="nofollow">Mei Shenghua;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Song Maoshuang&option=202" target="_blank" rel="nofollow">Song Maoshuang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kohlstedt David L.&option=202" target="_blank" rel="nofollow">Kohlstedt David L.;</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>State Key Laboratory of Isotope GeochemistryGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>CAS Key Laboratory for Experimental Study under Deep‐sea Extreme ConditionsInstitute of Deep‐sea Science and Engineering Chinese Academy of SciencesSanya China;</p> <p>State Key Laboratory of Isotope GeochemistryGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>Departments of Earth SciencesUniversity of Minnesota Twin CitiesMinneapolis MN 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=enstatite&option=203" rel="nofollow">enstatite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=diffusion creep&option=203" rel="nofollow">diffusion creep;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=water fugacity&option=203" rel="nofollow">water fugacity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle viscosity&option=203" rel="nofollow">mantle viscosity;</a> </p> <div class="translation"> 机译：enstatite;扩散蠕变;水坑;地幔粘度; </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/0704020652050.html">Diffusion Creep of Enstatite at High Pressures Under Hydrous Conditions</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Guinan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Guinan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mei Shenghua&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mei Shenghua,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Song Maoshuang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Song Maoshuang,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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