• 主题
高级搜索  >
历史搜索 清空历史
首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Structure of the oceanic lithosphere and upper mantle north of the Gloria Fault in the eastern mid‐Atlantic by receiver function analysis
【24h】

Structure of the oceanic lithosphere and upper mantle north of the Gloria Fault in the eastern mid‐Atlantic by receiver function analysis

机译：通过接收函数分析，在东部中大西洋中北方的海洋岩石圈和上部地幔的结构

获取原文
获取原文并翻译 | 示例
       
页面导航
  • 摘要
  • 著录项
  • 相似文献
  • 相关主题

摘要

Abstract >Receiver functions (RF) have been used for several decades to study structures beneath seismic stations. Although most available stations are deployed on shore, the number of ocean bottom station (OBS) experiments has increased in recent years. Almost all OBSs have to deal with higher noise levels and a limited deployment time (～1?year), resulting in a small number of usable records of teleseismic earthquakes. Here we use OBSs deployed as midaperture array in the deep ocean (4.5–5.5?km water depth) of the eastern mid‐Atlantic. We use evaluation criteria for OBS data and beamforming to enhance the quality of the RFs. Although some stations show reverberations caused by sedimentary cover, we are able to identify the Moho signal, indicating a normal thickness (5–8?km) of oceanic crust. Observations at single stations with thin sediments (300–400?m) indicate that a probable sharp lithosphere‐asthenosphere boundary (LAB) might exist at a depth of ～70–80?km which is in line with LAB depth estimates for similar lithospheric ages in the Pacific. The mantle discontinuities at ～410?km and ～660?km are clearly identifiable. Their delay times are in agreement with PREM. Overall the usage of beam‐formed earthquake recordings for OBS RF analysis is an excellent way to increase the signal quality and the number of usable events. </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：ID =“JGRB52265-ABS-ABS-0001”XML：Lang =“en”> <标题类型=“main”>抽象</ title> >接收器功能（RF）已使用几十年来学习地震站下面的结构。虽然大多数可用站部署在岸上，但近年来海底站（OBS）实验的数量增加。几乎所有Obs都必须处理更高的噪音水平和有限的部署时间（〜1？一年），导致少量可用的Telesmicic地震记录。在这里，我们使用东部中大西洋的深海（4.5-5.5英里）的米坡阵列的OBS。我们使用评估标准进行OBS数据和波束成形以增强RFS的质量。虽然一些站点表现出由沉积盖引起的混响，但我们能够识别Moho信号，表明海洋地壳的正常厚度（5-8 km）。单个站点的观察沉积物（300-400μm）表明可能存在尖锐的岩石圈 - 哮喘斜面边界（实验室）可能存在于〜70-80的深度〜70-80英里，这与实验室深度估计相同的类似岩石尺年在太平洋。 Mantle不连续〜410 km和〜660 km是明确可识别的。他们的延迟时间与Prem一致。总体而言，对OBS RF分析的光束形成的地震录制的使用是增加信号质量和可用事件数量的绝佳方法。</ 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-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24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=Hannemann Katrin&option=202" target="_blank" rel="nofollow">Hannemann Katrin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krüger Frank&option=202" target="_blank" rel="nofollow">Krüger Frank;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dahm Torsten&option=202" target="_blank" rel="nofollow">Dahm Torsten;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lange Dietrich&option=202" target="_blank" rel="nofollow">Lange Dietrich;</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>GEOMAR‐Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>Institute of Earth and Environmental ScienceUniversity of PotsdamPotsdam Germany;</p> <p>Institute of Earth and Environmental ScienceUniversity of PotsdamPotsdam Germany;</p> <p>GEOMAR‐Helmholtz Centre for Ocean Research KielKiel Germany;</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=receiver function&option=203" rel="nofollow">receiver function;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic lithosphere and mantle&option=203" rel="nofollow">oceanic lithosphere and mantle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ocean bottom seismology&option=203" rel="nofollow">ocean bottom seismology;</a> </p> <div class="translation"> 机译：接收器功能;海洋岩石圈和地幔;海底地震学; </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/0704020652037.html">Structure of the oceanic lithosphere and upper mantle north of the Gloria Fault in the eastern mid-Atlantic by receiver function analysis</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hannemann Katrin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hannemann Katrin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krueger Frank&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Krueger Frank,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dahm Torsten&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dahm Torsten,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. Biogeosciences .</a> <span>2017</span><span>,第10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：通过接收函数分析，在东部中大西洋中北方的海洋岩石圈和上部地幔的结构</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_detail_thesis/0204116774622.html">Seismic structure of the lithosphere and upper mantle beneath the ocean islands near mid-oceanic ridges</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=C.Haldar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">C.Haldar,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P.Kumar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">P.Kumar,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=M.Ravi Kumar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">M.Ravi Kumar </a> <a href="/journal-foreign-28367/" target="_blank" rel="nofollow" class="tuijian_authcolor">Solid Earth .</a> <span>2014</span><span>,第1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：大洋中脊附近海洋岛屿下方岩石圈和上地幔的地震构造</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024718246.html">Thickness of the oceanic crust, the lithosphere, and the mantle transition zone in the vicinity of the Tristan da Cunha hot spot estimated from ocean-bottom and ocean-island seismometer receiver functions</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wolfram H. Geissler&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wolfram H. Geissler,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilfried Jokat&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wilfried Jokat,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marion Jegen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Marion Jegen,</a> <a href="/journal-foreign-30366/" target="_blank" rel="nofollow" class="tuijian_authcolor">Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth .</a> <span>2017</span><span>,第期</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：海洋地壳的厚度，岩石圈和地幔过渡区在近海底和海洋岛地震表接收器功能估计的Tristan Da Cunha热点附近</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_fifth-european-conference-underwater-acoustics-ecua-2000-vol2-jul-10-13_thesis/020511586037.html">SIMULATION OF OCEAN ACOUSTIC TOMOGRAPHY IN THE NORTH EASTERN ATLANTIC</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=S. Bausson&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">S. Bausson,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=D. Mauuary&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">D. Mauuary </a> <a href="/conference-foreign-23565/" target="_blank" rel="nofollow" class="tuijian_authcolor">Fifth European Conference on Underwater Acoustics (ECUA 2000) Vol.2 Jul 10-13, 2000 Villeurbanne .</a> <span>2000</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：东北大西洋海洋声学层析成像的模拟</span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-degree-foreign_mphd_thesis/02061263160.html">The crustal and upper mantle shear velocity structure of Eastern North America from the joint inversion of receiver function and surface-wave dispersion.</a> <b>[D] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fnais, Mohammed Saeed.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fnais, Mohammed Saeed. </a> <span>2004</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：北美东部地壳和上地幔的剪切速度结构由接收函数和面波频散共同反演。</span> </p> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-journal-foreign-pmc_wiley-blackwell-online-open_thesis/040004966629.html">Predictions and Observations for the Oceanic Lithosphere From S‐to‐P Receiver Functions and SS Precursors</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Catherine A. Rychert&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Catherine A. Rychert,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nick Harmon&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Nick Harmon </a> <span>-1</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：从S到P的接收函数和SS前兆对海洋岩石圈的预测和观测</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/0100093674855.html ">Seismic structure of the lithosphere and upper mantle beneath the ocean islands near mid-oceanic ridges</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=C. Haldar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">C. Haldar,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=P. Kumar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">P. Kumar,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=M. Ravi Kumar&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">M. Ravi Kumar </a> <span>2014</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：大洋中脊附近海洋岛屿下岩石圈和上地幔的地震结构</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_ad_thesis/020711097163.html">Quantitative Analysis of Abyssal Hills in the Atlantic Ocean: A CorrelationBetween Axis Mantle Temperature and Extensional Faulting</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Goff, J. A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Goff, J. A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jaroslow, G. E.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jaroslow, G. E.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kleinrock, M. C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kleinrock, M. C.,</a> <span>1993</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：大西洋深海丘陵的定量分析：轴向地幔温度与伸展断层的相关性</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_earth-science-frontiers_thesis/0201253150215.html">吉林东部汪清新生代玄武岩中地幔包体的矿物化学:对该地区岩石圈地幔形成过程的启示</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=宋樾&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 宋樾</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王建&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王建</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘金霖&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘金霖</a> <span> <a href="/journal-cn-4911/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地学前缘 </a> </span> <span> . 2013</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geology-in-china_thesis/0201252104382.html">瑞雷-泰勒不稳定性与中国东部岩石圈——三论岩石圈地幔蘑菇云构造</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=袁学诚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 袁学诚</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李善芳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李善芳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=管烨&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,管烨</a> <span> <a href="/journal-cn-4800/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地质 </a> </span> <span> . 2012</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-sinica_thesis/0201252024234.html">安徽女山地幔橄榄岩捕虏体的同位素组成:中国东部新生代岩石圈地幔时代制约</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘志超&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘志超</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴福元&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吴福元</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=储著银&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,储著银</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2010</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_acta-petrologica-sinica_thesis/0201252033568.html">中国东部地幔橄榄岩捕虏体的Re-Os同位素地球化学:岩石圈地幔的形成年龄和减薄作用的制约</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=支霞臣&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 支霞臣</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=秦协&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,秦协</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2004</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geochimica_thesis/0201252984268.html">中国东部岩石圈地幔的演化——地幔岩捕虏体微量元素的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张明&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张明</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=解广轰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,解广轰</a> <span> <a href="/journal-cn-4899/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地球化学 </a> </span> <span> . 1996</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-14201_thesis/020221093889.html">I-型富集地幔与中国东部大陆岩石圈地幔演化</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周新华&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 周新华</a> <span> <a href="/conference-cn-14201/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2010年全国岩石学与地球动力学研讨会 </a> <span> <span> . 2010</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/02031614581.html">中国东部部分地区新生代岩石圈地幔的成因-微量元素和Sr-Nd-Os同位素制约</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=安亚军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 安亚军</a> <span> . 2011</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120210941733.html">一种海洋FPSO上部模块组合支撑结构</a> <b>[P]</b> . <span> 中国专利： CN210942162U </span> <span> . 2020.07.07</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120101241585.html">一种海洋FPSO上部模块组合支撑结构</a> <b>[P]</b> . <span> 中国专利： CN110406640A </span> <span> . 2019-11-05</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130458809852.html">automatic generation of a fault tree analysis for functional of a system from its description in structured analysis.</a> <b>[P]</b> . <span> 外国专利： <!-- --> ITTO930833A1 </span> <span> . 1995-05-06</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：根据结构化分析中的描述，自动生成用于系统功能的故障树分析。 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130461819258.html">automatic generation of a fault tree analysis for functional of a system from its description in structured analysis.</a> <b>[P]</b> . <span> 外国专利： <!-- --> ITTO930833D0 </span> <span> . 1993-11-05</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：根据结构化分析中的描述，自动生成用于系统功能的故障树分析。 </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('0704025591923','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="" 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"> <!-- <a href="javascript:void(0);" onclick="link_analysis('/shoppingcart/auth/list.html',this)">购物车</a>--> </li> <li class="yijian"> <a href="javascript:void(0);" onclick="link_analysis('/mycenter/auth/complaint.html',this)">意见反馈</a> </li> <li class="top"> <a href="javascript:scrollTo(0,0);">回到顶部</a> </li> <li class="shouye"> <a href="/">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">关于掌桥</a></li> <li><a href="/help/helpmap.html">资源导航</a></li> <li><a href="/help/helpguide.html">新手指南</a></li> <li><a href="/help/helpcenter.html">常见问题</a></li> <li><a href="/sitemap.html">网站地图</a></li> <li><a href="/help/helpcenter.html?type=9">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">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="0704025591923down" data-source="7," data-out-id="P0xF3IaKhSHDlAxLH3hYdtMKjh8A4dMwtqIbblVoqCZ0HUbaqXAYoCGYEZ6lR/x0," data-f-source-id="7" data-title="Structure of the oceanic lithosphere and upper mantle north of the Gloria Fault in the eastern mid‐Atlantic by receiver function analysis" data-price="20" data-site-name="" data-transnum="24" style="display:none;"></span> <input type="hidden" value="4" id="sourcetype"> <input type="hidden" value="34677" id="journalid"> <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="Structure of the oceanic lithosphere and upper mantle north of the Gloria Fault in the eastern mid‐Atlantic by receiver function analysis"/> <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=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/common.js?v=5.7.6"></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=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/tip.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/login.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/down.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/common/search.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/searchtype.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/user/regist.js?v=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/zxs_solor/detail.js?v=5.7.6"></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/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=5.7.6"></script> <script type="text/javascript" src="https://cdn.zhangqiaokeyan.com/js/weipu/weipu.js?v=5.7.6"></script> </body> <script> $(function(){ var weiPuStatus = getCookie('WeiPuStatus'); if(weiPuStatus){ tipWeiPuStatus(weiPuStatus); delCookie('WeiPuStatus'); } getFacetKeywordVoInId(); var sourcetype = $("#sourcetype").val(); if(sourcetype ==1||sourcetype==4){ getJournal(); } }) </script> </html>