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Shear Wave Splitting Beneath Eastern North American Continent: Evidence for a Multilayered and Laterally Variable Anisotropic Structure

机译：北北美洲大陆下面的剪力波分裂：多层和横向变差各向异性结构的证据

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Abstract > Eastern North America records a tectonic history of over 3?Ga in duration. Much of this record is preserved within the lithosphere and may be unraveled by detailed studies of its interior structure. Past episodes of tectonic activity likely left their imprints in the form of anisotropy‐forming rock fabric presently preserved in the lithosphere of the continent. We perform shear wave splitting measurements using observations of core‐refracted waves collected from a ~1,300‐km‐long array extending from James Bay in Quebec to the Fundy basin in Maine, with lateral spacing of 10–100?km between instruments. Close spacing of instruments helps us associate anisotropic properties with geological boundaries. We find that the fast polarizations concentrate between N60°E and N90°E with an average of N80°E and change systematically with backazimuth. In addition, we observe a lateral increase in delay time from 0.56? type="mathematics"> ±0.25? s at the NW end of the array to 0.9 type="mathematics"> 0?±?0.41? s at the SE end. The location of lateral change in delay time does not match geological boundaries on the surface but seems to match the geophysical boundary at depth of 160?km. We interpret this boundary in splitting values to be the edge of cratonic lithosphere at depth. Our observations suggest that the anisotropic structure beneath our study area is complex and possibly both multilayered and laterally variable. </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> > 东北美国持续时间超过3？GA的构造历史。在岩石圈内保存了大部分记录，可以通过对其内部结构的详细研究来解开。过去的构造活动剧集可能以目前在大陆的岩石圈的各向异性形成岩石面料的形式留下了印记。我们使用从Quebec在魁北克詹姆斯湾延伸到缅因州的Qames Bay队延伸的阵列中收集的核心折射波的观察，在缅因州的Quedy盆地，在仪器之间的横向间隔为10-100 km。仪器的近距离有助于我们将各向异性特性与地质边界相关联。我们发现快速偏振浓缩在N60°E和N90°E之间，平均为N80°E，并用基亚轴系统系统地改变。此外，我们观察0.56的延迟时间横向增加？ type =“mathematics”> ±0.25？ s </ i> </ span> 在数组的NW结尾到0.9 type =“mathematics”> 0？±？0.41？ s </ i> </ span> 在SE结束。延迟时间的横向变化的位置与地面上的地质边界不匹配，但似乎与160 km深度的地球物理边界匹配。我们将该边界解释在分裂值中，以深入的裂缝岩石圈的边缘。我们的观察结果表明，我们的研究区域下方的各向异性结构是复杂的，并且可能是多层和横向变量。 </ 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8期</span><b style="margin: 0 2px;">|</b><span>共15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=Chen Xiaoran&option=202" target="_blank" rel="nofollow">Chen Xiaoran;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Yiran&option=202" target="_blank" rel="nofollow">Li Yiran;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Levin Vadim&option=202" target="_blank" rel="nofollow">Levin Vadim;</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 Planetary SciencesRutgers UniversityPiscataway NJ USA;</p> <p>Department of Earth and Planetary SciencesRutgers UniversityPiscataway NJ USA;</p> <p>Department of Earth and Planetary SciencesRutgers UniversityPiscataway NJ 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;"> </p> </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/0704023360469.html">Shear Wave Splitting Beneath Eastern North American Continent: Evidence for a Multilayered and Laterally Variable Anisotropic Structure</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Xiaoran&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chen Xiaoran,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Yiran&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Yiran,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Levin Vadim&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Levin Vadim </a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第8期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：北北美洲大陆下面的剪力波分裂：多层和横向变差各向异性结构的证据</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704011034381.html">Shear wave splitting as a diagnostic of variable anisotropic structure of the upper mantle beneath central Fennoscandia</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=L. 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