Aseismic Motions Drive a Sparse Seismicity During Fluid Injections Into a Fractured Zone in a Carbonate Reservoir

机译：在碳酸盐储层的流体注入过程中，抗空疫苗在流体注入过程中驱动稀疏地震性

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Abstract >An increase in fluid pressure in faults can trigger seismicity and large aseismic motions. Understanding how fluid and faults interact is an essential goal for seismic hazard and reservoir monitoring, but this key relation remains unclear. We developed an in situ experiment of fluid injections at a 10?meter scale. Water was injected at high pressure in different geological structures inside a fault damaged zone, in limestone at 280?m depth in the Low Noise Underground Laboratory (France). Induced seismicity, as well as strains, pressure, and flow rate, was continuously monitored during the injections. Although nonreversible deformations related to fracture reactivations were observed for all injections, only a few tests generated seismicity. Events are characterized by a 0.5‐to‐4?kHz content and a small magnitude (approximately ?3.5). They are located within 1.5?m accuracy between 1 and 12?m from the injections. Comparing strain measurements and seismicity shows that more than 96% of the deformation is aseismic. The seismic moment is also small compared to the one expected from the injected volume. Moreover, a dual seismic behavior is observed as (1) the spatiotemporal distribution of some cluster of events is clearly independent from the fluid diffusion (2) while a diffusion‐type pattern can be observed for some others clusters. The seismicity might therefore appear as an indirect effect to the fluid pressure, driven by aseismic motion and related stress perturbation transferred through failure. </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”>摘要</ title> >故障中的流体压力的增加可以引发地震性和大的抗震运动。了解液体和故障互动是如何遭受地震危害和储层监测的基本目标，但这种关键关系仍然不明朗。我们开发了一个液体注射的原位试验，以10？米级。在低噪声地下实验室（法国）的280μm深度的石灰石中，在大型故障受损区内的不同地质结构的高压下注入水。在注射期间连续监测诱导的地震性，以及菌株，压力和流速。虽然对所有注射观察到与骨折再活化有关的不可转让的变形，但只有少数测试产生了地震性。事件的特征在于0.5至4 kHz含量和小幅度（约3.5）。它们位于1.5米的1到12米之间，从注射中介于1到12℃。比较应变测量和地震性表明，超过96％的变形是症态。与注射体积的预期相比，地震矩也很小。此外，观察到双地震行为为（1）一些事件的时空分布显然独立于流体扩散（2），同时可以针对一些其他簇观察扩散型图案。因此，由于失败转移的抗气运动和相关应激扰动驱动，地震性可能出现对流体压力的间接影响。</ 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-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20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=Duboeuf Laure&option=202" target="_blank" rel="nofollow">Duboeuf Laure;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=De Barros Louis&option=202" target="_blank" rel="nofollow">De Barros Louis;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cappa Frédéric&option=202" target="_blank" rel="nofollow">Cappa Frédéric;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guglielmi Yves&option=202" target="_blank" rel="nofollow">Guglielmi Yves;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deschamps Anne&option=202" target="_blank" rel="nofollow">Deschamps Anne;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Seguy Simon&option=202" target="_blank" rel="nofollow">Seguy Simon;</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>Université C?te d'Azur CNRS OCA IRD GéoazurSophia Antipolis France;</p> <p>Université C?te d'Azur CNRS OCA IRD GéoazurSophia Antipolis France;</p> <p>Université C?te d'Azur CNRS OCA IRD GéoazurSophia Antipolis France;</p> <p>Earth and Environmental Science AreaLawrence Berkeley National LaboratoryBerkeley CA USA;</p> <p>Université C?te d'Azur CNRS OCA IRD GéoazurSophia Antipolis France;</p> <p>Université Aix‐Marseille CNRS IRD CEREGEAix‐en‐Provence 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=induced seismicity&option=203" rel="nofollow">induced seismicity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid injections&option=203" rel="nofollow">fluid injections;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fractured zone&option=203" rel="nofollow">fractured zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=aseismic motions&option=203" rel="nofollow">aseismic motions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=meter‐scale in situ experiments&option=203" rel="nofollow">meter‐scale in situ experiments;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydromechanics&option=203" rel="nofollow">hydromechanics;</a> </p> <div class="translation"> 机译：诱导地震性;流体注射;裂缝区;抗震;仪表 - 尺度在原位实验;流体力学; </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/0704020651832.html">Aseismic Motions Drive a Sparse Seismicity During Fluid Injections Into a Fractured Zone in a Carbonate Reservoir</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Duboeuf Laure&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Duboeuf Laure,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=De Barros Louis&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">De Barros Louis,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cappa Frederic&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Cappa Frederic,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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