Apparent Splitting of SS Waves Propagating Through an Isotropic Lowermost Mantle

机译：表观分裂 s的波浪通过各向同性的最低型地幔传播

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Abstract > Observations of shear wave anisotropy are key for understanding the mineralogical structure and flow in the mantle. Several researchers have reported the presence of seismic anisotropy in the lowermost 150–250?km of the mantle (i.e., D <mat:math display="inline" altimg="urn:x-wiley:jgrb:media:jgrb52636:jgrb52636-math-0002" wiley:location="equation/jgrb52636-math-0002.png"> <mat:msup> <mat:mrow/> <mat:mrow> <mat:mi>′′</mat:mi> </mat:mrow> </mat:msup> </mat:math> layer), based on differences in the arrival times of vertically ( S V ) and horizontally ( S H ) polarized shear waves. By computing waveforms at a period > 6?s for a wide range of 1‐D and 3‐D Earth structures, we illustrate that a time shift (i.e., apparent splitting) between S V and S H may appear in purely isotropic simulations. This may be misinterpreted as shear wave anisotropy. For near‐surface earthquakes, apparent shear wave splitting can result from the interference of S with the surface reflection s S . For deep earthquakes, apparent splitting can be due to the S wave triplication in D <mat:math display="inline" altimg="urn:x-wiley:jgrb:media:jgrb52636:jgrb52636-math-0003" wiley:location="equation/jgrb52636-math-0003.png"> <mat:msup> <mat:mrow/> <mat:mrow> <mat:mi>′′</mat:mi> </mat:mrow> </mat:msup> </mat:math> , reflections off discontinuities in the upper mantle, and 3‐D heterogeneity. The wave effects due </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 =“JGRB52636-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> >剪切波各向异性的观察是关键了解矿物学结构和地幔的流动。几位研究人员报告了在地幔中最下面150-250？km的地震各向异性存在（即，D <MAT：MATH DISPLES =“内联”ALTIMG =“URN：X-WIley：JGRB：媒体：JGRB52636：JGRB52636- Math-0002“Wiley：Location =”等式/ JGRB52636-Math-0002.png“> <MAT：MSUP> <MAT：MROW /> <MAT：MROW> <MAT：MI>''</ MAT：MI> < / mat：mrow> </ mat：msup> </ mat：math>图层），基于垂直到达时间的差异（ s </ i> v </ i>）和水平（ S </ i> H </ i>）偏振剪切波。通过计算在宽范围的1-D和3-D接地结构的时段> 6？S的波形中，我们说明了 s v之间的时间偏移（即，表观分裂） </ i>和 s </ i> h </ i>可能出现在纯粹的各向同性模拟中。这可能被误解为剪切波各向异性。对于近表面地震，表观剪切波分裂可能是由 S </ i>的干扰，表面反射 S S </ i>。对于深海地震，表观分裂可以是由于D <MAT的 S </ i>波段，而MATH DISPLAY =“内联”ALTIMG =“URN：X-WIley：JGRB：媒体：JGRB52636：JGRB52636-数学-0003“Wiley：位置=”等式/ JGRB52636-Math-0003.png“> <MAT：MSUP> <MAT：MROW /> <MAT：MROW> <MAT：MI>'''</ MAT：MI> </ MAT：MROW> </ MAT：MSUP> </ MAT：数学>，反射上部地幔中的不连续性，以及3-D的异质性。波效应到期 </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>2018年第5期</span><b style="margin: 0 2px;">|</b><span>共14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=Parisi Laura&option=202" target="_blank" rel="nofollow">Parisi Laura;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferreira Ana M. G.&option=202" target="_blank" rel="nofollow">Ferreira Ana M. G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ritsema Jeroen&option=202" target="_blank" rel="nofollow">Ritsema Jeroen;</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>PSE DivisionKing Abdullah University of Science and TechnologyThuwal Saudi Arabia;</p> <p>Department of Earth SciencesUniversity College LondonLondon UK;</p> <p>Department of Earth and Environmental SciencesUniversity of MichiganAnn Arbor MI 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=shear wave splitting&option=203" rel="nofollow">shear wave splitting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=D' layer&option=203" rel="nofollow">D' layer;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle anisotropy&option=203" rel="nofollow">mantle anisotropy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=core‐mantle boundary&option=203" rel="nofollow">core‐mantle boundary;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lowermost mantle&option=203" rel="nofollow">lowermost mantle;</a> </p> <div class="translation"> 机译：剪切波分裂;D'层;地幔各向异性;核心地幔边界;最低地幔; </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/0704025592882.html">Apparent Splitting of <fi >S</fi>S Waves Propagating Through an Isotropic Lowermost Mantle</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Parisi Laura&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Parisi Laura,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferreira Ana M. 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