Earthquake Directivity, Orientation, and Stress Drop Within the Subducting Plate at the Hikurangi Margin, New Zealand

机译：新西兰Hikurangi边缘的底板板内的地震方向性，方向和压力下降

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Abstract > We develop an approach to calculate earthquake source directivity and rupture velocity for small earthquakes, using the whole source time function rather than just an estimate of the duration. We apply the method to an aftershock sequence within the subducting plate beneath North Island, New Zealand, and investigate its resolution. We use closely located, highly correlated empirical Green's function (EGF) events to obtain source time functions (STFs) for this well‐recorded sequence. We stack the STFs from multiple EGFs at each station, to improve the stability of the STFs. Eleven earthquakes ( <fi>M</fi> 3.3–4.5) have sufficient azimuthal coverage, and both <fi>P</fi> and <fi>S</fi> STFs, to investigate directivity. The time axis of each STF in turn is stretched to find the maximum correlation between all pairs of stations. We then invert for the orientation and rupture velocity of both unilateral and bilateral line sources that best match the observations. We determine whether they are distinguishable and investigate the effects of limited frequency bandwidth. Rupture orientations are resolvable for eight earthquakes, seven of which are predominantly unilateral, and all are consistent with rupture on planes similar to the main shock fault plane. Purely unilateral rupture is rarely distinguishable from asymmetric bilateral rupture, despite a good station distribution. Synthetic testing shows that rupture velocity is the least well‐resolved parameter; estimates decrease with loss of high‐frequency energy, and measurements are best considered minimum values. We see no correlation between rupture velocity and stress drop, and spatial stress drop variation cannot be explained as an artifact of varying rupture velocity. </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> >使用整体，开发一种方法来计算地震源方向性和破裂速度的方法，使用整体源时间函数而不是估计持续时间。我们将该方法应用于北岛，新西兰下面的底板板内的余震序列，并调查其分辨率。我们使用密切定位，高度相关的经验绿色功能（EGF）事件，以获得这种录制良好的序列的源时间函数（STF）。我们将STF堆叠在每个站的多个EGF中，以提高STF的稳定性。 11地震（<Fi> M </ Fi> 3.3-4.5）具有足够的方位角覆盖范围，以及<fi> p </ fi>和<fi> s </ fi> stf，以研究方向性。依次拉伸每个STF的时间轴以找到所有站对之间的最大相关性。然后，我们反转了最佳匹配观察的单边和双边线来源的方向和破裂速度。我们确定它们是否可区分并调查有限频率带宽的影响。破裂取向可解决八个地震，其中七个主要是单侧的，所有这些都是符合与主要冲击故障平面类似的平面破裂。尽管良好的车站分布，但纯粹是单边破裂的人很少可区分。合成测试显示破裂速度是最良好的解决方案;估计随着高频能量的损失而降低，并且测量最佳被认为是最小值。我们认为破裂速度和应力下降之间没有相关性，并且不能解释空间应力下降变化作为不同破裂速度的伪影。 </ p> </ abstract> </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=Abercrombie Rachel E.&option=202" target="_blank" rel="nofollow">Abercrombie Rachel E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Poli Piero&option=202" target="_blank" rel="nofollow">Poli Piero;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bannister Stephen&option=202" target="_blank" rel="nofollow">Bannister Stephen;</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 EnvironmentBoston UniversityBoston MA USA;</p> <p>Department of EarthAtmospheric and Planetary Sciences MITCambridge MA USA;</p> <p>GNS ScienceLower Hutt New Zealand;</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=earthquake&option=203" rel="nofollow">earthquake;</a> </p> <div class="translation"> 机译：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/0704025592059.html">Earthquake Directivity, Orientation, and Stress Drop Within the Subducting Plate at the Hikurangi Margin, New Zealand</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Abercrombie Rachel E.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Abercrombie Rachel E.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Poli Piero&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Poli Piero,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bannister Stephen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bannister Stephen </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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class="tuijian_auth tuijian_authcolor"> . 王勤彩</a> <span> . 2000</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120112406340.html">方向性电磁钢板用原板、成为方向性电磁钢板用原板的材料的方向性硅钢板、方向性电磁钢板用原板的制造方法及方向性电磁钢板的制造方法</a> <b>[P]</b> . <span> 中国专利： CN112437818A </span> <span> . 2021-03-02</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/061203644644.html">通过使用耦合环内的电极来控制边缘区域中的离子的方向性的系统和方法</a> <b>[P]</b> . <span> 中国专利： CN107527785B </span> <span> . 2020.02.28</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130406761398.html">seismic protective structure for protection of a plate partition, plate partition, parts kit for construction of a seismic protective structure, method for protection of a plate partition against a given level of seismic stress and method for restoring a plate partition after an earthquake</a> <b>[P]</b> . <span> 外国专利：  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