首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Acoustic Reflectivity From Variously Oriented Orthorhombic Media: Analogies to Seismic Responses From a Fractured Anisotropic Crust
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Acoustic Reflectivity From Variously Oriented Orthorhombic Media: Analogies to Seismic Responses From a Fractured Anisotropic Crust

机译:来自各种定向的正交介质的声学反射率:与裂缝各向异性地壳的地震反应类别

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Abstract >The variations in the strength of seismic reflections with both angles of incidence and azimuth are being used to constrain the orientations and degrees of mechanical anisotropy of geological formations. This information is often used in turn to infer the directions of fracturing and stress usually assuming simplified geological structures that in many cases are not realistic. In order to further understand this problem, the reflectivities from a set of variously titled samples cut from a single block of a common anisotropic composite material are measured with both angles of incidence and azimuth in the laboratory. Each sample is analogous to a formation in which the fracture sets increasingly dip. The observed responses differ from plane wave theory due to the finite nature of the experiment. However, the deviations are well accounted for by modeling the acoustic reflectivity using its bounded pulse. As expected, the reflectivities vary with the sample tilt, the angle of incidence, and the azimuth at which the measurements are made. However, some of these responses, such as the precritical reflectivities, do not appear to strongly vary with azimuth for a given sample. Critical angle phenomena, too, must be used cautiously as the observed reflectivity peaks do not lie at the exact critical angle. These results suggest that reflectivities could be an important source of information with regard to the spatial orientation of anisotropic layer. </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> >争斗的抗震性强度的变化和方位角和方位角的抗震性的变化约束地质形成的方向和机械各向异性程度。该信息通常反过来使用通常假设在许多情况下的简化地质结构的压裂和压力的方向不逼真。为了进一步理解该问题,通过实验室中的入射和方位角的两个角度测量来自单个常见的各向异性复合材料的一组不同标题的样品的反射率。每个样品类似于裂缝组越来越倾斜的形成。由于实验的有限性,所观察到的响应与平面波理论不同。然而,通过使用其有界脉冲建模声学反射率来归因于偏差。正如预期的那样,反射率随着样品倾斜,入射角和测量的方位角而变化。然而,其中一些响应,例如前临界反射症,对于给定样本的方位角似乎没有强烈变化。临界角现象也必须小心地使用,因为观察到的反射率峰不会呈现为确切的临界角度。这些结果表明,反思活动可能是关于各向异性层的空间取向的重要信息来源。</ 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12期</span><b style="margin: 0 2px;">|</b><span>共17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=Malehmir Reza&option=202" target="_blank" rel="nofollow">Malehmir Reza;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmitt Douglas R.&option=202" target="_blank" rel="nofollow">Schmitt Douglas R.;</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 PhysicsUniversity of AlbertaEdmonton Alberta Canada;</p> <p>Department of PhysicsUniversity of AlbertaEdmonton Alberta Canada;</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=phenolic&option=203" rel="nofollow">phenolic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ultrasonic&option=203" rel="nofollow">ultrasonic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=anisotropy&option=203" rel="nofollow">anisotropy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=reflectivity&option=203" rel="nofollow">reflectivity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic&option=203" rel="nofollow">seismic;</a> </p> <div class="translation"> 机译:酚醛;超声波;各向异性;反射率;地震; </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/0704025591103.html">Acoustic Reflectivity From Variously Oriented Orthorhombic Media: Analogies to Seismic Responses From a Fractured Anisotropic Crust</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Malehmir Reza&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Malehmir Reza,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmitt Douglas R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Schmitt Douglas R. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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href="/patent-detail/06120103409041.html">一种正交各向异性介质流体因子与裂缝参数反演方法</a> <b>[P]</b> . <span> 中国专利: CN110687601A </span> <span> . 2020-01-14</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/061203306708.html">一种预测正交各向异性介质裂缝强度的方法</a> <b>[P]</b> . <span> 中国专利: CN107797142B </span> <span> . 2019.05.07</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130409802581.html">Fracture characterization by interferometric drillbit imaging, time reversal imaging of fractures using drill bit seismics, and monitoring of fracture generation via time reversed acoustics and electroseismics</a> <b>[P]</b> . <span> 外国专利: <!-- 美国专利: --> US9678236B2 </span> <span> . 2017-06-13</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:通过干涉式钻头成像,使用钻头地震法对裂缝进行时间反转成像以及通过时间反演的声学和电震监测裂缝生成来表征裂缝 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130420642830.html">FRACTURE CHARACTERIZATION BY INTERFEROMETRIC DRILLBIT IMAGING, TIME REVERSAL IMAGING OF FRACTURES USING DRILL BIT SEISMICS, AND MONITORING OF FRACTURE GENERATION VIA TIME REVERSED ACOUSTICS AND ELECTROSEISMICS</a> <b>[P]</b> . <span> 外国专利: <!-- 美国专利: --> US2013116926A1 </span> <span> . 2013-05-09</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:干涉法钻探成像,利用钻头地震对断裂的时间逆向成像,以及通过时间反演的电和电学监测断裂的产生来表征断裂 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130424741426.html">FRACTURE CHARACTERIZATION BY INTERFEROMETRIC DRILLBIT IMAGING, TIME REVERSAL IMAGING OF FRACTURES USING DRILL BIT SEISMICS, AND MONITORING OF FRACTURE GENERATION VIA TIME REVERSED ACOUSTICS AND ELECTROSEISMICS</a> <b>[P]</b> . <span> 外国专利: <!-- 世界知识产权组织专利: --> WO2011136760A1 </span> <span> . 2011-11-03</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:干涉法钻探成像,利用钻头地震对断裂的时间逆向成像,以及通过时间反演的电和电学监测断裂的产生来表征断裂 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704025591103','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="" 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