首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Coherent Seismic Arrivals in the PP Wave Coda of the 2012 M _w M _ww ?7.2 Sumatra Earthquake: Water Reverberations or an Early Aftershock?

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Coherent Seismic Arrivals in the PP Wave Coda of the 2012 M _w M _ww ?7.2 Sumatra Earthquake: Water Reverberations or an Early Aftershock?

机译：2012 m _{w m _{w w？7.2苏门答腊地震：水混响或早期余震？}}

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Abstract > Teleseismic records of the 2012? M <sub> w </sub> ?7.2 Sumatra earthquake contain prominent phases in the P wave train, arriving about 50 to 100?s after the direct P arrival. Azimuthal variations in these arrivals, together with back‐projection analysis, led Fan and Shearer ([Fan, W., 2016a], <url href="https://doi.org/10.1002/2016GL067785">https://doi.org/10.1002/2016GL067785</url> ) to conclude that they originated from early aftershock(s), located ～150 km northeast of the mainshock and landward of the trench. However, recently, Yue et al. ([Yue, H., 2017], <url href="https://doi.org/10.1002/2017GL073254">https://doi.org/10.1002/2017GL073254</url> ) argued that the anomalous arrivals are more likely water reverberations from the mainshock, based mostly on empirical Green's function analysis of a M 6 earthquake near the mainshock and a water phase synthetic test. Here we present detailed back‐projection and waveform analyses of three M 6 earthquakes within 100?km of the M <sub> w </sub> ?7.2 earthquake, including the empirical Green's function event analyzed in Yue et al. ([Yue, H., 2017], <url href="https://doi.org/10.1002/2017GL073254">https://doi.org/10.1002/2017GL073254</url> ). In addition, we examine the waveforms of three M 5.5 reverse‐faulting earthquakes close to the inferred early aftershock location in Fan and Shearer ([Fan, W., 2016a], <url href="https://doi.org/10.1002/2016GL067785">https://doi.org/10.1002/2016GL067785</url> ). These results suggest that the reverberatory character of the anomalous arrivals i </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 =“JGRB52644-ABS-ABS-ABS-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> > 2012的Telesmic记录？ m </ i> <sub> w </ s> </ sub>？7.2 sumatra地震含有突出的阶段在 p </ i>波动列车中，到达50到100？s在直接的 p </ i>到达后。这些抵达的方位而振变化，以及背投分析，LED风扇和剪切器（[风扇，W.，2016A]，<URL HREF =“HTTPS://Doi.org/10.1002 / 2011G1067785”> HTTPS：// DOI .org / 10.1002 / 2016GL067785 </ URL>）得出结论，它们起源于余震早期，位于大约150公里的主屏幕和沟渠的陆地。然而，最近，岳等人。（[yue，H.，2017]，<url href =“https://doi.org/10.1002/2017GL073254”> https://doi.org/10.1002/2017GL073254 </ URL>）认为异常抵达来自主歇地的水混响更多的是，主要是在主屏蔽附近的A> M </ i> 6地震的经验绿色功能分析和水相合成试验。在这里，我们在 m </ i> <subl <s sub的 </ sub的</ sub中，呈现三个 m </ i> 6地震的详细的回投影和波形分析。 >？7.2地震，包括在yue等人分析的经验绿色的功能事件。（[yue，H.，2017]，<url href =“https://doi.org/10.1002/2017gl073254”> https://doi.org/10.1002/2017GL073254 </ URL>）。此外，我们检查三个 m </ i> 5.5反向断层地震的波形，靠近风扇和剪切机的推断早期余震位置（[粉丝，W.，2016a]，<url href =“https： //doi.org/10.1002/20101Ag1067785“> https://doi.org/10.1002/20101Ag1067785 </ URL>）。这些结果表明，异常到达的混响性质我 </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4期</span><b style="margin: 0 2px;">|</b><span>共13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=Fan Wenyuan&option=202" target="_blank" rel="nofollow">Fan Wenyuan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shearer Peter M.&option=202" target="_blank" rel="nofollow">Shearer Peter M.;</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>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Scripps Institution of OceanographyUniversity of California San DiegoLa Jolla CA 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;"> </p> </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/0704025592014.html">Coherent Seismic Arrivals in the <fi >P</fi>P Wave Coda of the 2012 <fi > M <sub>w</sub> </fi> M <sub >w</sub>w ?7.2 Sumatra Earthquake: Water Reverberations or an Early Aftershock?</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fan Wenyuan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fan Wenyuan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shearer Peter M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Shearer Peter M. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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Coherent Seismic Arrivals in the PP Wave Coda of the 2012 M w M ww ?7.2 Sumatra Earthquake: Water Reverberations or an Early Aftershock?

摘要

Coherent Seismic Arrivals in the PP Wave Coda of the 2012 M _w M _ww ?7.2 Sumatra Earthquake: Water Reverberations or an Early Aftershock?