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Rock Strength and Texture Evolution During Deformation in the Earth's Ductile Lithosphere: A Two‐Phase Thermodynamics Model

机译：地球延性岩石圈变形过程中的岩石力量和纹理演变：一种两相热力学模型

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Abstract >Building upon the two‐phase and grain damage theory, we propose a new formulation allowing to track the evolution of phase mixing/segregation during ductile deformation of a two‐phased aggregate. Our model is based on a set of variables characterizing a rock texture: the mean grain sizes and the phase proportion. During ductile deformation, activation of different micromechanical processes impacts the aggregate texture. Dislocation and diffusion creep are the two main deformation processes considered. We only account for the effect of Zener pinning in slowing down grain growth and allow for active grain‐size reduction mechanisms in the diffusion creep domain. For this purpose, an equation is proposed to track the phase mixing evolution during ductile deformation. Numerical application using anorthite rheology shows that any grain reduction mechanisms that could be active in the diffusion creep regime requires a very high partition fraction in order to reach the grain size predicted by the feldspar piezometer. Application of this model to gabbroic composition, relevant for the ductile crust, demonstrates that the strong coupling between phases grain sizes and interface evolution results in steady‐state grain sizes far below the field boundary. This effect is coeval with an important increase of mixing between the two phases. In addition, accounting for the phase mixing results in a drop of the global aggregate stress during deformation. This model allows for further comparison of mylonitized textures evolution with natural shear zones at the local and regional scales. </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”XML：ID =“GGGE21802-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> >在两相和晶粒损伤理论上，我们提出了一种新的配方，允许追踪双相聚集体的延性变形期间相混合/偏析的演变。我们的模型基于一组变量，表征岩石纹理：平均晶粒尺寸和相位比例。在延展性变形期间，不同微机械过程的激活会影响聚集体纹理。错位和扩散蠕变是考虑的两个主要变形过程。我们仅考虑了齐纳钉扎在缩小谷物生长中的影响，并允许扩散蠕变结构域中的主动晶粒尺寸减少机制。为此目的，提出了一种等式，以跟踪延展性变形期间的相位混合演化。使用钙高流变学的数值应用表明，在扩散蠕变状态下可以有效的任何谷物还原机制需要非常高的分隔壁，以便到达由长石压电计预测的晶粒尺寸。该模型在与韧性地壳相关的铲发组合物中的应用表明，相粒尺寸和界面演化之间的强耦合导致远低于场边界的稳态晶粒尺寸。这种效果是辛伐安，两相之间的混合的重要增加。此外，核对相混合导致变形过程中的全局聚集应力下降。该模型允许在本地和区域尺度的自然剪切区进一步比较米隆型纹理演变。</ 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>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共43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=Bevillard Benoit&option=202" target="_blank" rel="nofollow">Bevillard Benoit;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Richard Guillaume&option=202" target="_blank" rel="nofollow">Richard Guillaume;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Raimbourg Hugues&option=202" target="_blank" rel="nofollow">Raimbourg Hugues;</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>Institut des Sciences de la Terre d'Orléans UMR 7327 CNRS/Université d'Orléans 1A rue de la FérollerieOrléans Cedex 2 France;</p> <p>Institut des Sciences de la Terre d'Orléans UMR 7327 CNRS/Université d'Orléans 1A rue de la FérollerieOrléans Cedex 2 France;</p> <p>Institut des Sciences de la Terre d'Orléans UMR 7327 CNRS/Université d'Orléans 1A rue de la FérollerieOrléans Cedex 2 France;</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=two‐phase rheology&option=203" rel="nofollow">two‐phase rheology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=phase mixing&option=203" rel="nofollow">phase mixing;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ductile deformation&option=203" rel="nofollow">ductile deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=strain localization&option=203" rel="nofollow">strain localization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mylonite textures&option=203" rel="nofollow">mylonite textures;</a> </p> <div class="translation"> 机译：两相流变学;相混合;韧性变形;应变定位;米隆岩纹理; 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Л.ВС</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王勋弟&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王勋弟</a> <span> <a href="/journal-cn-50777/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地质地球化学 </a> </span> <span> . 1994</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201296060544.html">扬子克拉通东北缘岩石圈地幔的Re-Os同位素地球化学:大陆岩石圈地幔的形成和演化的制约</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=支霞臣&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 支霞臣</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=L.Reisberg&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,L.Reisberg</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=彭子成&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,彭子成</a> <span> <a href="/journal-cn-57400/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿物岩石地球化学通报 </a> </span> <span> . 2001</span><span>,第4期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_jilin-geology_thesis/0201253943102.html">地球岩石圈的演化机制：兼论开普勒动力导致岩石圈演化谱</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=牛广林&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 牛广林</a> <span> <a href="/journal-cn-4983/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 吉林地质 </a> </span> <span> . 1995</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-31042_thesis/02022259999.html">扬子克拉通东北缘岩石圈地幔的Re-Os同位素地球化学:大陆岩石圈地幔的形成和演化的制约</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=支霞臣&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 支霞臣</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=L.Reisberg&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,L.Reisberg</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=彭子成&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,彭子成</a> <span> <a href="/conference-cn-31042/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第七届全国同位素地质年代学同位素地球化学学术讨论会 </a> <span> <span> . 2001</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020316045771.html">辽西中生代岩石圈地幔特征：义县组玄武岩中捕虏晶的矿物学和地球化学制约</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=许瑶&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 许瑶</a> <span> . 2020</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120213090380.html">一种研究岩石圈构造变形过程及其形成机制的实验平台</a> <b>[P]</b> . <span> 中国专利： CN213150122U </span> <span> . 2021-05-07</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120112743060.html">岩石圈构造变形物理模拟实验装置及实验方法</a> <b>[P]</b> . <span> 中国专利： CN112781519A </span> <span> . 2021-05-11</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130416591224.html">Tectonic model of seismic zones in the continental lithosphere of the earth. METHOD OF CONSTRUCTION AND USE OF MODELS tectonic seismic zones in the continental lithosphere EARTH</a> <b>[P]</b> . <span> 外国专利：  RU2013116281A </span> <span> . 2014-10-20</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：地球大陆岩石圈地震带的构造模型。大陆岩石圈地球构造地震带模型的构建和使用方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130412227461.html">Methods for generating a model of a physical entity, to render a model, to create a tree of hierarchical data, to rotate the data to model the lithosphere of the earth, and to build trees from data, computer software, apparatus, processing and conversion of data, the network. System for implementing the method.</a> <b>[P]</b> . <span> 外国专利：  BRPI0917572A2 </span> <span> . 2015-11-17</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：用于生成物理实体模型，渲染模型，创建分层数据树，旋转数据以对地球岩石圈建模以及从数据，计算机软件，设备，处理和转换中构建树的方法数据，网络。用于实现该方法的系统。 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130478576647.html">Screwdriver made from high strength steel strip - which is inserted into ductile steel tube with deformations in wall to grip handle</a> <b>[P]</b> . <span> 外国专利：  DE2828077A1 </span> <span> . 1980-01-10</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：由高强度钢带制成的螺丝刀-插入易变形的钢管中，壁上会变形以握紧手柄 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: 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