Stress Orientations in a Locked Subduction Zone at the Southern Hikurangi Margin, New Zealand

机译：新西兰南部的南部苏兰提锁定区的应力取向

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Abstract > We analyze the orientation of the stress field in the southern Hikurangi subduction zone, New Zealand, using focal mechanism inversions, <fi>S</fi> wave splitting fast directions, and gravitational stresses. Here the oceanic Pacific plate is being obliquely subducted beneath the continental Australian plate in the New Zealand plate boundary zone. The study makes use of 399 earthquakes for focal mechanism inversion and 425 earthquakes for shear wave splitting analysis, located with a network of seismic stations spanning southern North Island. We distinguish between stresses in the Pacific plate (from focal mechanism inversion) and Australian plate (from <fi>S</fi> wave fast directions) and gravitational stresses, in three regions: Western, Central Basin, and Eastern. In the Western region, the principal axis of horizontal compression (SHmax) is oriented NE‐SW, parallel to the margin, in the upper Australian and lower Pacific plate. In the Central Basin, SHmax in the Australian plate is oriented NW‐SE, perpendicular to the margin; in the lower subducting Pacific plate SHmax is oriented NE‐SW. In the Eastern region, SHmax is oriented NE‐SW in the upper plate, while in the lower plate there is a change in orientation to NNW‐SSE. We interpret the stress orientations of the lower plate in the Western and Central Basin regions as a consequence of bending of the subducting plate. Sources of upper Australian plate stresses are likely to be bending stresses, gravitational stresses, and tectonic loading, with differing relative magnitudes across the study area. </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> >我们分析了新西兰南部Hikurangi俯冲区的应力场的方向焦点机制逆，<fi> s </ fi>波分裂快速方向，以及引力应力。在这里，海洋太平洋板块在新西兰板材边界区的大陆澳大利亚板块下方倾斜化。该研究利用399次地震进行焦点机制反演和425个地震，用于剪力波分析分析，遍布北岛南部南部的地震站网络。我们区分太平板（从焦点机制反转）和澳大利亚板块（从<fi> s </ fi>波快速方向）和引力应力，在三个地区：西部，中央盆地和东部。在西部地区，水平压缩的主要轴线（Shmax）是面向上澳大利亚和下太平的边缘的Ne-SW，平行于边缘。在中央盆地中，澳大利亚板块的Shmax面向垂直于边缘的NW-SE;在较低的窗玻璃太平洋板Shmax是面向Ne-SW的。在东部地区，Shmax在上板上取向Ne-Sw，而在下板中有方向的变化为NNW-SSE。由于弯曲板的弯曲，我们解释了西部和中央盆地区域的下板的应力取向。上部澳大利亚板块的来源可能是弯曲应力，引力应力和构造负载，在研究区域上具有不同的相对幅度。 </ 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10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=Evanzia Dominic&option=202" target="_blank" rel="nofollow">Evanzia Dominic;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilson Thomas&option=202" target="_blank" rel="nofollow">Wilson Thomas;</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=Lamb Simon&option=202" target="_blank" rel="nofollow">Lamb Simon;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hirschberg Hamish&option=202" target="_blank" rel="nofollow">Hirschberg Hamish;</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;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oblique subduction&option=203" rel="nofollow">oblique subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=stress&option=203" rel="nofollow">stress;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SHmax&option=203" rel="nofollow">SHmax;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=anisotropy&option=203" rel="nofollow">anisotropy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=gravitational stresses&option=203" rel="nofollow">gravitational stresses;</a> </p> <div class="translation"> 机译：倾斜俯冲;压力;Shmax;各向异性;引力应力; </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/0704020651553.html">Stress Orientations in a Locked Subduction Zone at the Southern 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=Evanzia Dominic&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Evanzia Dominic,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilson Thomas&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wilson Thomas,</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" class="tuijian_auth tuijian_authcolor">Savage Martha K.,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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