Moho Depths of Antarctica: Comparison of Seismic, Gravity, and Isostatic Results

Pappa F.; Ebbing J.; Ferraccioli F.

摘要

Abstract >The lithospheric structure of Antarctica is still underexplored. Moho depth estimate studies are in disagreement by more than 10?km in several regions, including, for example, the hinterland of the Transantarctic Mountains. Taking account the sparseness of seismological stations and the nonuniqueness of potential field methods, inversions of Moho depth are performed here based on satellite gravity data in combination with currently available seismically constrained Moho depth estimates. Our results confirm that a lower density contrast at the Moho is present under East Antarctica than beneath West Antarctica. A comparison between the Moho depth derived from our inversion and an Airy‐isostatic Moho model also reveals a spatially variable buoyancy contribution from the lithospheric mantle beneath contrasting sectors of East Antarctica. Finally, to test the plausibility of different Moho depths scenarios for the Transantarctic Mountains‐Wilkes Subglacial Basin system, we present 2‐D lithospheric models along the Trans‐Antarctic Mountain Seismic Experiment/Gamburtsev Mountain Seismic experiment seismic profile. Our models show that if a moderately depleted lithospheric mantle of inferred Proterozoic age underlies the region, then a shallower Moho is more likely beneath the Wilkes Subglacial Basin. If however, refertilization processes occurred in the upper mantle, for example, in response to Ross‐age subduction, then a deeper Moho scenario is preferred. We conclude that 3‐D lithospheric modeling, coupled with the availability of new seismic information in the hinterland of the Transantarctic Mountains, is required to help resolve this controversy, thereby also reducing the ambiguities in geothermal heat flux estimation beneath this key part of the East Antarctic Ice Sheet. </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> >南极的岩石结构仍然是缺乏光泽的。 Moho Depth估计研究在几个地区的分歧中有超过10千米，包括例如Transantarctic山脉的腹地。考虑到地震站的稀疏性和潜在的场方法的非感性，基于卫星重力数据，与当前可用的地震限制的Moho深度估计相结合，在这里进行Moho深度的逆。我们的结果证实，Moho的较低密度对比度在东南南极洲而不是西南南极洲。从我们的反演和通风 - 等静电Moho模型的Moho深度之间的比较也揭示了来自东南南极地区的岩石罩的空间可变的浮力贡献。最后，为了测试不同Moho深度的合理性，为Transantarctic Mountains-Wilkes子彩色盆地系统提供2-D型岩石山地地震实验/ Gamburtsev Mountain Seismic Experiment Acisismic简介的2-D岩石型模型。我们的模型表明，如果推断前古代的中等耗尽的岩石型壁龛是该地区的下潜，那么较浅的Moho更容易在威尔克斯底部盆地下方。然而，如果响应于罗斯时代俯冲，则在上部地幔中发生引用过程，则优选更深的Moho场景。我们得出结论，3-D型岩体建模，加上Transantarctic山脉腹地中的新地震信息的可用性，以帮助解决这一争议，从而减少了东部的这一关键部分下面的地热热通量估计中的模糊性南极冰盖。</ 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3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=Pappa F.&option=202" target="_blank" rel="nofollow">Pappa F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ebbing J.&option=202" target="_blank" rel="nofollow">Ebbing J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferraccioli F.&option=202" target="_blank" rel="nofollow">Ferraccioli F.;</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 GeosciencesKiel UniversityKiel Germany;</p> <p>Department of GeosciencesKiel UniversityKiel Germany;</p> <p>British Antarctic SurveyCambridge UK;</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=Antarctica&option=203" rel="nofollow">Antarctica;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Moho&option=203" rel="nofollow">Moho;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=gravity&option=203" rel="nofollow">gravity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=inversion&option=203" rel="nofollow">inversion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithosphere&option=203" rel="nofollow">lithosphere;</a> </p> <div class="translation"> 机译：南极洲;moho;重力;反演;岩石圈; </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/0704023360347.html">Moho Depths of Antarctica: Comparison of Seismic, Gravity, and Isostatic Results</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pappa F.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pappa F.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ebbing J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ebbing J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ferraccioli F.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ferraccioli F. </a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2019</span><span>,第3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：南极洲的Moho深度：地震，重力和等静力结果的比较</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-seismology-english-edition_thesis/0201252694432.html">The gravity and isostatic Moho in North China Craton and their implications to seismicity</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yangfan Deng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yangfan Deng,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Weiming Fan&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Weiming Fan,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhongjie Zhang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhongjie Zhang,</a> <a href="/journal-foreign-4884/" target="_blank" rel="nofollow" class="tuijian_authcolor">地震学报（英文版） .</a> <span>2014</span><span>,第002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：华北克拉通的重力和静力莫霍面及其对地震活动的影响</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_journal-applied-geodesy_thesis/0204112327581.html">Towards the Moho depth and Moho density contrast along with their uncertainties from seismic and satellite gravity observations</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Abrehdary Majid&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Abrehdary Majid,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sjöberg Lars E.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sjöberg Lars E.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bagherbandi Mohammad&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bagherbandi Mohammad,</a> <a href="/journal-foreign-903/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of applied geodesy .</a> <span>2017</span><span>,第4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：走向莫霍面深度和莫霍面密度对比，以及来自地震和卫星重力观测的不确定性</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_meeting-286811_thesis/0705015038124.html">A comparison of different isostatic models applied to satellite gravity gradiometry</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=F. Wild&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">F. Wild,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=B. Heck&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">B. Heck,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=International Association of Geodesy(IAG)&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">International Association of Geodesy(IAG) </a> <a href="/conference-foreign-286811/" target="_blank" rel="nofollow" class="tuijian_authcolor">IAG International Symposium on Gravity, Geoid and Space Missions .</a> <span>2005</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：应用于卫星重力梯度的不同等效模型的比较</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061694485.html">The relationship between crustal density and volcanic rocks in the western United States including a comparison of isostatic compensation techniques for gravity data correction</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Garinger, Linda Pickett&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Garinger, Linda Pickett </a> <span>2008</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：美国西部地壳密度与火山岩之间的关系，包括用于重力数据校正的等静压补偿技术的比较</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_detail_thesis/040006209615.html">A recovered Moho model by integrated inversion of gravity and seismic depths in Iran</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sahar Ebadi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sahar Ebadi,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Abdolreza Safari&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Abdolreza Safari,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Riccardo Barzaghi&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Riccardo Barzaghi,</a> <span>2020</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：通过对伊朗重力和地震深度进行综合反演得到的恢复的Moho模型</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000128669472.html">Moho Depths of Antarctica: Comparison of Seismic, Gravity, and Isostatic Results</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=F. Pappa&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">F. Pappa,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=J. Ebbing&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">J. Ebbing,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=F. Ferraccioli&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">F. Ferraccioli </a> <span>2019</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：南极洲的Moho深度：地震，重力和等静力结果的比较</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-geodaetica-cartographica-sinica_thesis/0201278732767.html">基于卫星重力场模型反演全球及区域Moho面深度</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈文进&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 陈文进</a> <span> <a href="/journal-cn-27765/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 测绘学报 </a> </span> <span> . 2020</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-geodesy-geodynamics_thesis/0201252718130.html">利用EGM2008重力数据反演中国大陆Moho深度</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=玄松柏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 玄松柏</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=申重阳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,申重阳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=谈洪波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,谈洪波</a> <span> <a href="/journal-cn-4886/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 大地测量与地球动力学 </a> </span> <span> . 2015</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-seismological-research_thesis/0201253309146.html">考虑沉积层重力改正的中国西部Moho面深度反演</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=姜永涛&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 姜永涛</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张永志&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,张永志</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王帅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王帅</a> <span> <a href="/journal-cn-4924/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地震研究 </a> </span> <span> . 2015</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_china-earthquake-engineering-journal_thesis/0201254340326.html">地震与海啸作用下重力式岸墙旋转位移拟静力分析</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=林永亮&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 林永亮</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李新星&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李新星</a> <span> <a href="/journal-cn-5027/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地震工程学报 </a> </span> <span> . 2015</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_china-earthquake-engineering-journal_thesis/0201254340498.html">地震与海啸作用下重力式岸墙旋转位移拟静力分析</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=林永亮1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 林永亮1</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李新星2&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李新星2</a> <span> <a href="/journal-cn-5027/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地震工程学报 </a> </span> <span> . 2015</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-33960_thesis/02022996602.html">用近垂直地震反射信息比较研究全球Moho的基本特征</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=杨宝俊&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 杨宝俊</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘财&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘财</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=孙加鹏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,孙加鹏</a> <span> <a href="/conference-cn-33960/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地球物理学会第14届年会 </a> <span> <span> . 1998</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314844305.html">高水位填埋场静力与地震稳定性超重力离心模型试验研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李俊超&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李俊超</a> <span> . 2018</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061203292858.html">一种从深度域地震数据中提取深度域地震子波的方法</a> <b>[P]</b> . <span> 中国专利： CN106873038B </span> <span> . 2019.05.03</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120109380395.html">一种从深度域地震数据中提取深度域地震子波的方法</a> <b>[P]</b> . <span> 中国专利： CN106873038A </span> <span> . 2017-06-20</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130405052661.html">HOW MUCH SPECIFIC GRAVITY OF HIGGS BOSON AND UNIVERSE IS; HOW MUCH ATTRACTIVE FORCE GENERATED BY VISIBLE SUBSTANCES AND ATTRACTIVE FORCE GENERATED BY DARK MATTER IN UNIVERSE ARE; AND COMPARISON IN ELECTRON LOVE REVOLUTION ORBIT, ELECTRON LOVE MASS ENERGY, ELECTRON LOVE MASS, ELECTRON LOVE SIZE, ELECTRON LOVE VOLUME, ELECTRON LOVE SPECIFIC GRAVITY, MAGNETIC PHOTON ENERGY PER SECOND GENERATED BY ELECTRON LOVE, AND INTER-ELECTRON-LOVE ATTRACTIVE FORCE, BETWEEN GROUND SURFACE AND UNIVERSE, UNDERGROUND OF EARTH, AND DEPTH OF SUN</a> <b>[P]</b> . <span> 外国专利：  JP2019088068A </span> <span> . 2019-06-06</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：希格斯玻色子和宇宙的比重是多少？宇宙中可见物质产生的吸引力和暗物质产生的吸引力如何？和在电子爱因特所产生的每一个电子爱因数的变化中，对电子爱的旋转轨道，电子爱的质量能量，电子爱的质量，电子爱的大小，电子爱的体积，电子爱的比重，电子光子能量的每秒钟产生的电子爱的旋转轨道进行比较。地面和宇宙，地球的地下和太阳的深度 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130405568500.html">Method for building velocity models for pre-stack depth migration via the simultaneous joint inversion of seismic, gravity and magnetotelluric data.</a> <b>[P]</b> . <span> 外国专利：  EP2667224B1 </span> <span> . 2019-08-07</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：通过地震，重力和大地电磁数据的同时联合反演建立叠前深度偏移速度模型的方法。 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130409285301.html">METHOD FOR BUILDING VELOCITY MODELS FOR PRE-STACK DEPTH MIGRATION VIA THE SIMULTANEOUS JOINT INVERSION OF SEISMIC, GRAVITY AND MAGNETOTELLURIC DATA</a> <b>[P]</b> . <span> 外国专利：  NO340762B1 </span> <span> . 2017-06-12</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：通过地震，重力和地磁数据的同时联合反演建立叠前深度迁移速度模型的方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360347','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" style="display: none"> <div class="journal-sub"> <h2>期刊订阅</h2> <img src="https://cdn.zhangqiaokeyan.com/img/loginclose.png" alt="关闭" onclick="$('.journalsub-pop-up').hide()"> <p class="pardon">抱歉，该期刊暂不可订阅，敬请期待！</p> <p class="current">目前支持订阅全部北京大学中文核心（2020）期刊目录。</p> <div style="display: flex;margin-top: 69px;justify-content: space-between;"> <div class="no-sub" onclick="$('.journalsub-pop-up').hide()">暂不订阅</div> <div class="other-sub" onclick="continueSub('from=pc-detail')">继续订阅其他期刊</div> </div> </div> </div> <div class="right_btn"> <ul> <li class="gouwuche">  </li> <li class="yijian"> <a href="javascript:void(0);" onclick="link_analysis('/mycenter/auth/complaint.html',this)" title="意见反馈">意见反馈</a> </li> <li class="top"> <a href="javascript:scrollTo(0,0);" title="回到顶部">回到顶部</a> </li> <li class="shouye"> <a href="/" title="首页">回到首页</a> </li> </ul> </div> <div class="xllindexfooter"> <div class="xllindexfootercenter"> <div class="xllindexfooterleft left" > <div class="xllindexfooterleftli"> <ul> <li><a href="/about.html" title="关于掌桥">关于掌桥</a></li> <li><a href="/help/helpmap.html" title="资源导航">资源导航</a></li> <li><a href="/help/helpguide.html" title="新手指南">新手指南</a></li> <li><a href="/help/helpcenter.html" title="常见问题">常见问题</a></li> <li><a href="/sitemap.html" title="网站地图">网站地图</a></li> <li><a href="/help/helpcenter.html?type=9" title="版权声明">版权声明</a></li> </ul> </div> <div class="xllindexfooterleft"> <p class="xllindexfooterlefteamil">客服邮箱：kefu@zhangqiaokeyan.com</p> <div class="xllindexfooterlefttcp"> <div class="xllindexfooterpoliceiimg"></div> <div class="xllindexfooterpoliceispan"> <span>京公网安备：11010802029741号 </span> <span>ICP备案号：<a href="https://beian.miit.gov.cn" rel="nofollow" target="_blank" title="ICP备案号">京ICP备15016152号-6</a></span> <span>六维联合信息科技 (北京) 有限公司©版权所有</span> </div> </div> </div> </div> <div class="xllindexfooterright left"> <ul> <li> <p style="font-weight: bold;">客服微信</p> <div></div> </li> <li> <p style="font-weight: bold;">服务号</p> <div></div> </li> </ul> </div> </div> </div> <span id="0704023360347down" data-source="7," data-out-id="4KJwuJLmMF5b9toPFZXBUNSvvt17eYNwN+P0+syhgdHsqmsuqPvH5xTz5cup//H8," data-f-source-id="7" data-title="Moho Depths of Antarctica: Comparison of Seismic, Gravity, and Isostatic Results" data-price="20" data-site-name="" data-transnum="24" style="display:none;"></span> <input type="hidden" value="4" id="sourcetype"> <input type="hidden" value="23285" id="journalid"> <input type="hidden" value="1" id="inyn_provide_service_level"> <input type="hidden" value="https://cdn.zhangqiaokeyan.com" id="imgcdn"> <input type="hidden" value="1" id="isdeatail"> <input type="hidden" value="" id="syyn_indexed_database"> <input type="hidden" value="" id="servicetype"> <input type="hidden" id="pagename" value="Moho Depths of Antarctica: Comparison of Seismic, Gravity, and Isostatic Results"/> <input type="hidden" value="thesis_get_original" id="pageIdentification"> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery-1.12.4.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/lwlh_ajax.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zq.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/jquery.cookie.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/top.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/newmail.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.7.8"></script> <script type="text/javascript" src="https://www.zhangqiaokeyan.com/statistics/static/pagecollection.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/tj.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/sse.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/pushbaidu.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/history.js"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/util/cookie.js?v=5.7.8"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.7.8"></script> </body> <script> $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); var inyn_provide_service_level = $("#inyn_provide_service_level").val(); if((sourcetype ==1||sourcetype==4)&&inyn_provide_service_level!=4){ getJournal(); } }) </script> </html>