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首页> 外文期刊>Geochemistry, geophysics, geosystems >Roughness Characteristics of Oceanic Seafloor Prior to Subduction in Relation to the Seismogenic Potential of Subduction Zones
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Roughness Characteristics of Oceanic Seafloor Prior to Subduction in Relation to the Seismogenic Potential of Subduction Zones

机译：与俯冲区郊区划分前海洋海底的粗糙度特征

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Abstract > We have developed a new approach to characterize the seafloor roughness seaward of the trenches, as a proxy for estimating the roughness of the subduction interface. We consider that abrupt elevation changes over given wavelengths play a larger role in the seismogenic behavior of the subduction interface than the amplitude of bathymetric variations alone. The new database, SubRough, provides roughness parameters at selected spatial wavelengths. Here we mainly discuss the spatial distribution of short‐ (12–20?km) and long‐wavelength (80–100?km) roughness, R <sub>SW</sub> and R <sub>LW</sub> , respectively, along 250‐km‐wide strips of seafloor seaward of the trenches. Compared with global trend, seamounts show distinct roughness signature of much larger amplitudes at both wavelengths, whereas aseismic ridges only differ from the global trend at long wavelengths. Fracture zones cannot be distinguished from the global trend, which suggests that their potential effect on rupture dynamics is not the consequence of their roughness, at least not at these wavelengths. Based on R <sub>LW</sub> amplitude, segments along subduction zones can be defined from rough to smooth. Subduction zones like the Solomons or the Ryukyus appear dominantly rough, whereas others like the Andes or Cascadia are dominantly smooth. The relative contribution of smooth versus rough areas in terms of respective lateral extents probably plays a role in multipatch rupture and thus in the final earthquake magnitude. We observe a clear correlation between high seismic coupling and relatively low roughness and conversely between low seismic coupling and relatively high seafloor roughness. </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> > 我们开发了一种新方法来表征沟渠的海底粗糙度，作为用于估计俯冲界面粗糙度的代理。我们认为，在给定波长上突然的升降改变在俯冲界面的发震行为中比单独的碱基变化的幅度发挥着更大的作用。新数据库亚级，在所选空间波长下提供粗糙度参数。在这里，我们主要讨论短（12-20 km）和长波长（80-100 km）粗糙度的空间分布， R </ I> <sub> sw </ sub> 和 R </ I> <sub> lw </ sub> 分别沿着250公里宽的沟渠沿着沟渠的海底沿线。与全球趋势相比，Seamounts在两个波长上显示出明显的粗糙度特征，在两个波长上具有更大的振幅，而抗震脊仅与长波长的全球趋势不同。骨折区域不能区分全球趋势，这表明它们对破裂动力学的潜在影响不是它们粗糙度的后果，至少不在这些波长处。基于 R </ I> <sub> lw </ sub> 幅度，沿俯冲区域的段可以从粗糙度定义为平滑。像所罗门或琉球等俯冲区显得庞大，而其他人像安第斯山户或级联人一样占据了庞大光滑。在各个横向范围方面，平滑与粗糙区域的相对贡献可能在多次破裂中起作用，因此在最终的地震幅度中起作用。我们观察到高地震耦合和相对低的粗糙度之间的明显相关性，相反在低地震耦合和相对高的海底粗糙度之间。 </ p> </摘要> </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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2018年第7期</span><b style="margin: 0 2px;">|</b><span>共26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=Lallemand Serge&option=202" target="_blank" rel="nofollow">Lallemand Serge;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peyret Michel&option=202" target="_blank" rel="nofollow">Peyret Michel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rijsingen Elenora&option=202" target="_blank" rel="nofollow">Rijsingen Elenora;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arcay Diane&option=202" target="_blank" rel="nofollow">Arcay Diane;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heuret Arnauld&option=202" target="_blank" rel="nofollow">Heuret Arnauld;</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>Géosciences Montpellier CNRS Montpellier UniversityMontpellier France;</p> <p>Géosciences Montpellier CNRS Montpellier UniversityMontpellier France;</p> <p>Géosciences Montpellier CNRS Montpellier UniversityMontpellier France;</p> <p>Géosciences Montpellier CNRS Montpellier UniversityMontpellier France;</p> <p>Géosciences Montpellier Guyane UniversityCayenne France;</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=seafloor roughness&option=203" rel="nofollow">seafloor roughness;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=proxy&option=203" rel="nofollow">proxy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction interface&option=203" rel="nofollow">subduction interface;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=wavelength&option=203" rel="nofollow">wavelength;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rupture dynamics&option=203" rel="nofollow">rupture dynamics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction earthquake&option=203" rel="nofollow">subduction earthquake;</a> </p> <div class="translation"> 机译：海底粗糙度;代理;俯冲界面;波长;破裂动力学;俯冲地震; 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