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首页> 外文期刊>Geophysical Research Letters >Estimate of the Rigidity of Eclogite in the Lower Mantle From Waveform Modeling of Broadband SS ‐to‐ PP Wave Conversions
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Estimate of the Rigidity of Eclogite in the Lower Mantle From Waveform Modeling of Broadband SS ‐to‐ PP Wave Conversions

机译：浅谈宽带波形建模eClogite在较低地幔中的刚性 S-TO- P P波转换

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Abstract > Broadband USArray recordings of the 21 July 2007 western Brazil earthquake ( M <sub> w </sub> =6.0; depth = 633?km) include high‐amplitude signals about 40?s, 75?s, and 100?s after the P wave arrival. They are consistent with S wave to P wave conversions in the mantle beneath northwestern South America. The signal at 100?s, denoted as S <sub>1750</sub> P , has the highest amplitude and is formed at 1,750?km depth based on slant‐stacking and semblance analysis. Waveform modeling using axisymmetric, finite difference synthetics indicates that S <sub>1750</sub> P is generated by a 10?km thick heterogeneity, presumably a fragment of subducted mid‐ocean ridge basalt in the lower mantle. The negative polarity of S <sub>1750</sub> P is a robust observation and constrains the shear velocity anomaly δ V <sub> S </sub> of the heterogeneity to be negative. The amplitude of S <sub>1750</sub> P indicates that δ V <sub> S </sub> is in the range from ?1.6% to ?12.4%. The large uncertainty in δ V <sub> S </sub> is due to the large variability in the recorded S <sub>1750</sub> P amplitude and simplifications in the modeling of S <sub>1750</sub> P waveforms. The lower end of our estimate for </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 =“grl56669-abs-abs-0001”> <标题类型=“main”>抽象</ title> > 2007年7月21日的宽带Usarray录音巴西地震（ m </ i> <sub> w </ i> </ sub> = 6.0;深度= 633 km）包括大约40？s，75？s的高幅度信号，在 p </ i>波浪到达后100？s之后。它们与南美洲西北部地幔中的波浪转换相一致，与 s 波浪相一致。在100·s的信号下表示为 s </ i> <sub> 1750 </ sub> p </ i>，具有最高幅度，并且基于倾斜的1,750 km深度形成堆叠和外观分析。使用轴对称的波形建模，有限差异合成表示 s </ i> <sub> 1750 </ sub> p </ i>由10Ωkm厚的异质性产生，大概是下压制的中间的片段-ocean山脊玄武岩在较低的地幔中。 s </ i> <sub> 1750 </ sub> p </ i>的负极性是一种稳健的观察，并限制剪切速度异常δ v <sub> s </ s> </ sub>的异质性为负。 s <s s <sub> 1750 </ sub> p </ i>表示δ</ i> v </ i> <sub> <i > S </ i> </ sub>在Δ1.6％的范围内为12.4％。 δ</ i> v </ i> <sum> s s </ sup>是由于记录的 s </ ch的巨大变异性i> <sub> 1750 </ sub> p 在建模中的幅度和简化，在 s </ i> <sub> 1750 </ sub> p </ i>波形中。我们估计的下端 </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第23期</span><b style="margin: 0 2px;">|</b><span>共7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=Haugland Samuel M.&option=202" target="_blank" rel="nofollow">Haugland Samuel M.;</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> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kaneshima Satoshi&option=202" target="_blank" rel="nofollow">Kaneshima Satoshi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thorne Michael S.&option=202" target="_blank" rel="nofollow">Thorne Michael S.;</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 Earth and Environmental SciencesUniversity of MichiganAnn Arbor MI USA;</p> <p>Department of Earth and Environmental SciencesUniversity of MichiganAnn Arbor MI USA;</p> <p>Department of Earth and Planetary SciencesKyushu UniversityFukuoka Japan;</p> <p>Department Geology and GeophysicsUniversity of UtahSalt Lake City UT 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=eclogite&option=203" rel="nofollow">eclogite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S ‐ P conversion&option=203" rel="nofollow">S ‐ P conversion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction&option=203" rel="nofollow">subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic crust&option=203" rel="nofollow">oceanic crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=stishovite&option=203" rel="nofollow">stishovite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismology&option=203" rel="nofollow">seismology;</a> </p> <div class="translation"> 机译：Eclogite;S - P转换;俯冲;海洋地壳;脊柱岩;地震学; 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