The Potential for Metamorphic Thermal Pulses to Develop During Compaction‐Driven Fluid Flow

Tian Meng; Ague Jay J.; Chu Xu; Baxter Ethan F.; Dragovic Nora; Chamberlain C. Page; Rumble Douglas

摘要

Abstract > Compaction‐driven fluid flow below the brittle‐ductile transition may be a means of transporting fluids during metamorphism. In particular, when a decompaction weakening mechanism is introduced to account for the rock viscosity reduction due to fluid overpressures, channeling instabilities evolve into high‐porosity/permeability fluid conduits that focus mass and energy transfer. In this study, we consider a crustal rheology that accounts simultaneously for upward‐increasing viscosity and decompaction weakening to examine the nucleation and evolution of fluid channelization in two dimensions (2‐D). The model shows that plume‐shaped flow patterns can develop on time scales as short as 10 4 years, during which the plume tails act as fluid conduits and the plume heads act as fluid dispersion zones near the brittle‐ductile transition. Collection of fluids into conduits is accomplished by a basal fluid catchment zone characterized by strong lateral fluid pressure gradients but low porosity/permeability. Relatively narrow ranges of viscous activation energy (～100 kJ mol ?1 ) and decompaction weakening factor (～10 ?4 ) are constrained if the fluid conduits are of kilometer scale in width. Significant thermal excursions (～65?°C) can be induced if a high flow rate, potentially from rapid intermittent dehydration, is realized within channels. Moreover, if the focused fluids emanate from external anomalously hot sources (e.g., magma intrusion), thermal pulses (100°C), and steep lateral temperature gradients (50°C km ?1 ) can be generated. Given the focusing efficiency estimated from our 2‐D compaction model, simple 3‐D modeling further shows that tubular conduits have the potential to cause thermal pulses 200°C within 10 4 years. </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”> <标题类型=“main”>抽象</ title> > 压实驱动的流体流量低于脆性 - 延展转变可以是在变质期间运输流体的方法。特别地，当引入分解弱化机理以考虑由于流体过度压力引起的岩石粘度降低时，通道稳定性发展成焦点和能量转移的高孔隙率/渗透性流体管道。在这项研究中，我们考虑了同时叙述的地壳流变学，用于向上增加粘度和分解削弱，以检查两个维度（2-D）中流体通道化的成核和演化。该模型表明，羽毛状的流动模式可以在短至10的时间尺度上发展 4 </ sup> 多年来，羽毛尾部充当流体管道，羽流头作为脆性延展转变附近的流体分散区。流体集合进入导管的基础流体集水区，其特征在于强横向流体压力梯度，但孔隙率/渗透率低。相对窄的粘性激活能量范围（〜100kJ摩尔？1 </ sup> ）和分解弱化因子（〜10 ？4 </ sup> 如果流体导管宽度的尺度是公正的尺度，则受到约束。如果在通道内实现高流量，可能会诱导显着的热偏移（〜65°C）（〜65Ω°C）。此外，如果聚焦的流体从外部异常热源（例如，岩浆侵入），热脉冲（＆ 100°C）散发出来，并且陡峭的横向温度梯度（＆ 50°C）？1 </ sup> ）可以生成。鉴于从我们的二维压实模型估计的聚焦效率，简单的3-D模型进一步表明，管状导管有可能导致热脉冲和GT; 200°C 4 </ sup> 年。 </ 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>2018年第1期</span><b style="margin: 0 2px;">|</b><span>共25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=Tian Meng&option=202" target="_blank" rel="nofollow">Tian Meng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ague Jay J.&option=202" target="_blank" rel="nofollow">Ague Jay J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chu Xu&option=202" target="_blank" rel="nofollow">Chu Xu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Baxter Ethan F.&option=202" target="_blank" rel="nofollow">Baxter Ethan F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dragovic Nora&option=202" target="_blank" rel="nofollow">Dragovic Nora;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chamberlain C. Page&option=202" target="_blank" rel="nofollow">Chamberlain C. Page;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rumble Douglas&option=202" target="_blank" rel="nofollow">Rumble Douglas;</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 Geology and GeophysicsYale UniversityNew Haven CT USA;</p> <p>Department of Geology and GeophysicsYale UniversityNew Haven CT USA;</p> <p>Department of Geology and GeophysicsYale UniversityNew Haven CT USA;</p> <p>Department of Earth and Environmental SciencesBoston CollegeBoston MA USA;</p> <p>Department of Earth and EnvironmentBoston UniversityBoston MA USA;</p> <p>Department of Earth System ScienceStanford UniversityStanford CA USA;</p> <p>Geophysical LaboratoryCarnegie Institution of WashingtonWashington DC 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=thermal pulse&option=203" rel="nofollow">thermal pulse;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=two‐phase flow&option=203" rel="nofollow">two‐phase flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=decompaction weakening&option=203" rel="nofollow">decompaction weakening;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid channelization&option=203" rel="nofollow">fluid channelization;</a> </p> <div class="translation"> 机译：热脉冲;两相流动;分解弱化;流体通道化; </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/0704023360424.html">The Potential for Metamorphic Thermal Pulses to Develop During Compaction‐Driven Fluid Flow</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tian Meng&option=202" target="_blank" rel="nofollow" class="tuijian_auth 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