Variations in Seismogenic Thickness Along the Central Alpine Fault, New Zealand, Revealed by a Decade's Relocated Microseismicity

Michailos Konstantinos; Smith Euan G.C.; Chamberlain Calum J.; Savage Martha K.; Townend John

摘要

Abstract > The Alpine Fault is an oblique strike‐slip fault that is known to fail in large magnitude (M7–8) earthquakes, yet it is currently seismically quiescent. We examine the low‐magnitude earthquake activity occurring along the central portion of the Alpine Fault using seismic data from five temporary seismic networks deployed for various lengths of time between late 2008 and early 2017. Starting from continuous seismic data, we detect earthquake arrivals and construct the longest and most extensive microearthquake catalog for the central Alpine Fault region to date, containing 9,111 earthquakes. This enables us to study the distribution and characteristics of the seismicity in unprecedented detail. Earthquake locations are constrained by high‐quality automatic and manual picks, and we perform relocations using waveform cross‐correlation to better constrain hypocenters. We have derived a new local magnitude scale calibrated by <fi>M</fi> <sub> <fi>w</fi> </sub> values. Magnitudes range between <fi>M</fi> <sub> <fi>L</fi> </sub> ?1.2 and 4.6, and our catalog is complete above <fi>M</fi> <sub> <fi>L</fi> </sub> 1.1. Earthquakes mainly occur southeast of the Alpine Fault (in the hanging wall) and exhibit low magnitudes. We observe a lack of seismicity beneath Aoraki/Mount Cook, which we associate with high uplift rates and high heat flow. Seismogenic cutoff depths vary along the strike of the Alpine Fault from 8?km, beneath the highest topography, to 20?km in the adjacent areas. </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”XML：ID =“GGGE21774-ABS-ABS-ABS-ABS-ABS”> <标题类型=“main”>抽象</ title> > Alpine Fault是一个倾斜的滑动故障，已知在大量（M7-8）地震中失败，但它目前正在地震静态。我们使用从部署的五个临时地震网络的地震数据来检查沿着高山故障的中央部分发生的低幅度地震活动，从部署于2008年底和2017年初。从连续地震数据开始，我们检测地震到达和构建迄今为止，中央阿尔卑斯山故障区域的最长和最广泛的微心地震目录，含有9,111地震。这使我们能够研究前所未有的细节中地震性的分布和特征。地震位置受到高质量的自动和手动选择的限制，我们使用波形交叉相关来进行重新定位与更好的限制低速度。我们派生了一种校准的新的局部幅度级 <fi> m </ fi> <sub> <fi> w </ fi> </ sub> 价值观。大小之间的范围 <fi> m </ fi> <sub> <fi> l </ fi> </ sub> ？1.2和4.6，我们的目录在上面完成 <fi> m </ fi> <sub> <fi> l </ fi> </ sub> 1.1。地震主要出现在高山故障（在悬挂墙上）的东南部，表现出低位。我们遵守Aoraki / Mount Cook的缺乏地震性，我们与高隆起速率和高热流相关联。脱离截止深度沿着高山故障的击球，在最高的地形下，在相邻区域的最高地形下的8 km击中，到20 km。 </ 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>2019年第1期</span><b style="margin: 0 2px;">|</b><span>共17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=Michailos Konstantinos&option=202" target="_blank" rel="nofollow">Michailos Konstantinos;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Smith Euan G.C.&option=202" target="_blank" rel="nofollow">Smith Euan G.C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chamberlain Calum J.&option=202" target="_blank" rel="nofollow">Chamberlain Calum J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Savage Martha K.&option=202" target="_blank" rel="nofollow">Savage Martha K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Townend John&option=202" target="_blank" rel="nofollow">Townend John;</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 Geography Environment and Earth SciencesVictoria University of WellingtonWellington New Zealand;</p> <p>School of Geography Environment and Earth SciencesVictoria University of WellingtonWellington New Zealand;</p> <p>School of Geography Environment and Earth SciencesVictoria University of WellingtonWellington New Zealand;</p> <p>School of Geography Environment and Earth SciencesVictoria University of WellingtonWellington New Zealand;</p> <p>School of Geography Environment and Earth SciencesVictoria University of WellingtonWellington 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;"> </p> </li> </ul> </div> </div> <div class="literature cardcommon"> 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