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Limitations of the Resolvability of Finite‐Fault Models Using Static Land‐Based Geodesy and Open‐Ocean Tsunami Waveforms

机译：利用静态陆地大地测地和开放海啸波形的有限故障模型可解义的限制

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Abstract >Finite‐fault inversions are a common technique, employed following large earthquakes, used to understand the nature of slip along a fault. Using multiple data sets, including static offsets from geodetic instruments and tsunami wave heights from open‐ocean gauges, a richer perspective on the expected slip distribution than using a singular tool is created. However, the model resolution obtained from open‐ocean tsunami data and techniques used to subsample that data have not been widely evaluated. Static geodetic data can provide near‐complete model resolution of the subduction megathrust near the trench, if data are local. However, model resolution falls off precipitously as distance between instrument and fault increases when geodetic data are limited to more distal on‐land sites. Tsunami data derived from open‐ocean waveforms are less dependent on station to fault distance, but offshore model resolution is lost due to necessary data processing, such as windowing, often necessary to avoid coastal reflections. This primarily affects the resolution in the downdip direction, which often arrives at open‐ocean stations later in the waveform. Spatial detail is also limited by the minimum subfault size that will satisfy the longwave approximation, which is dependent on the water depth. For most cases, this subfault limit is approximately 20 by 20?km. In many environments, the sparsity of offshore geodetic instruments, and the large distances between estimated slip and coastal geodetic gauges, makes the inclusion of open‐ocean data, if available, highly advantageous. Still it is possible even with the pairing of on‐land and offshore data sets for poorly resolved zones to exist. In these cases further resolution can be recovered through the incorporation of additional data sets such as strong‐motion data and seismic waveforms through a seismic‐geodetic inversion. < </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> >有限故障反转是一种常见的技术，在大地震之后采用，用于了解性质滑倒沿着故障。使用多个数据集，包括从开放海洋仪表的大地测量仪器和海啸波高的静态偏移，创建了比使用奇异工具的预期滑动分布的更丰富的透视图。然而，从开放海啸的数据和技术中获得的模型分辨率，用于将该数据尚未被广泛评估。如果数据是本地数据，静态大地测量数据可以在沟槽附近提供近端的模型分辨率。然而，当大地测量数据限于更多远端地点时，模型分辨率随着仪器之间的距离而急剧下降。来自开放海洋波形的海啸数据较少依赖于站到故障距离，但由于必要的数据处理，例如窗口，通常需要避免沿海反射，海上模型分辨率丢失。这主要影响下级方向的分辨率，这通常到达稍后在波形中的开放海洋站。空间细节也受到最小子故障尺寸的限制，该尺寸可以满足长波近似，这取决于水深。对于大多数情况而言，该子集限额约为20×20 km。在许多环境中，海上大地测量仪器的稀疏性以及估计的滑动和沿海大地线虫仪之间的大距离，包括开放海洋数据，如果有的话，非常有利。仍然是可能的，即使是陆地和近海数据集的配对，也可以存在不良分辨的区域。在这些情况下，可以通过通过地震 - 大地测量反转掺入诸如强运动数据和地震波形的附加数据集来恢复进一步的分辨率。</ p> < </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10期</span><b style="margin: 0 2px;">|</b><span>共16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=Williamson Amy L.&option=202" target="_blank" rel="nofollow">Williamson Amy L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Newman Andrew V.&option=202" target="_blank" rel="nofollow">Newman Andrew V.;</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>School of Earth and Atmospheric SciencesGeorgia Institute of TechnologyAtlanta GA USA;</p> <p>School of Earth and Atmospheric SciencesGeorgia Institute of TechnologyAtlanta GA 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=finite fault&option=203" rel="nofollow">finite fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=resolution&option=203" rel="nofollow">resolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tsunami&option=203" rel="nofollow">tsunami;</a> </p> <div class="translation"> 机译：有限故障;分辨率;海啸; </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/0704025591530.html">Limitations of the Resolvability of Finite‐Fault Models Using Static Land‐Based Geodesy and Open‐Ocean Tsunami Waveforms</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Williamson Amy L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Williamson Amy L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Newman Andrew V.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Newman Andrew V. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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