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首页> 外文期刊>Geochemistry, geophysics, geosystems >Directional change during a MM iocene RR ‐ NN geomagnetic polarity reversal recorded by mafic lava flows, SS heep CC reek RR ange, north central NN evada, USAUSA
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Directional change during a MM iocene RR ‐ NN geomagnetic polarity reversal recorded by mafic lava flows, SS heep CC reek RR ange, north central NN evada, USAUSA

机译:一个定向变化 M M. Iocene. R R. - n n Mafic Lava流动记录的地磁极性逆转, s s h C C. 雷克 R R. 北京北部 n n 埃文达, 美国美国

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Abstract >Recurring transitional field directions during three Miocene geomagnetic reversals provide evidence that lateral inhomogeneity of the lower mantle affects flow in the outer core. We compare new paleomagnetic results from a composite sequence of 15.2 Ma lava flows in north central Nevada (Sheep Creek Range; 40.7°N, 243.2°E), erupted during a polarity reversal, to published data from Steens Mountain (250 km to the northwest in Oregon) and the Newberry Mountains (650 km to the south in California) that document reversals occurring millions of years and many polarity switches earlier. Alternating field demagnetization, followed by thermal demagnetization in half the samples, clearly isolated the primary thermoremanent magnetization of Sheep Creek Range flows. We correlated results from our three sampled sections to produce a composite record that begins with a single virtual geomagnetic pole (VGP) at low latitude in the Atlantic, followed by two VGPs situated near latitude 30°N in NE Africa. After jumping to 83°N (one VGP), the pole moves to equatorial South America (one VGP), back to NE Africa (three VGPs), to high southern latitudes (two VGPs), back to equatorial South America (three VGPs), and finally to high northern latitudes (nine VGPs). The repeated visits of the transitional VGP to positions in South America and near NE Africa, as well as the similar behavior recorded at Steens Mountain and the Newberry Mountains, suggest that lower mantle or core‐mantle boundary features localize core flow structures, thereby imparting a discernible regional structure on the transitional geomagnetic field that persists for millions of years. </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”> <标题类型=“main”>抽象</ title> 在三个中间烯磁性逆转期间的重复过渡场方向提供了较低地幔的横向不均匀性影响外芯的流动。我们将新的古物磁性结果与北部内华达州北部(绵羊溪范围; 40.7°N,243.2°E)进行了比较了15.2 mA熔岩流量的综合序列,以在极性逆转期间爆发,从Steens Mountain(250公里到西北250公里)在俄勒冈州)和纽棕榈山(加利福尼亚州的650公里)将逆转逆转,早些时多数多年来,许多极性开关。交替的场地退磁,然后在样品的一半中进行热退磁,清楚地分离出羊溪范围流的主要热化磁化。我们与我们三个采样部分的相关结果相关,以产生一个在大西洋中低纬度的单个虚拟地磁杆(VGP)开始的复合记录,然后位于Ne Africa中的纬度30°N附近的两个VGP。跳到83°N(一个VGP)后,杆向赤道南美(一VGP)移动,回到Ne Africa(三个VGP),高南部纬度(两个VGPS),返回赤道南美(三个VGPS) ,最后到北纬度(九个VGPS)。过渡的VGP在南美洲和尼非附近的职位的重复访问,以及在Steens Mountain和Newberry山上记录的类似行为,表明较低的地幔或核心地幔边界具有定位核心流动结构,从而赋予在持续数百万年的过渡地磁场上可辨别的区域结构。</ 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>2017年第9期</span><b style="margin: 0 2px;">|</b><span>共19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=Bogue S. W.&option=202" target="_blank" rel="nofollow">Bogue S. W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Glen J. M. G.&option=202" target="_blank" rel="nofollow">Glen J. M. G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jarboe N. A.&option=202" target="_blank" rel="nofollow">Jarboe N. A.;</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 GeologyOccidental CollegeLos Angeles California USA;</p> <p>U.S. Geological Survey MS 989Menlo Park California USA;</p> <p>Scripps Institution of Oceanography University of California San DiegoLa Jolla California 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;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleomagnetism&option=203" rel="nofollow">paleomagnetism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geomagnetic&option=203" rel="nofollow">geomagnetic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=reversal&option=203" rel="nofollow">reversal;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=transition&option=203" rel="nofollow">transition;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Miocene&option=203" rel="nofollow">Miocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Nevada&option=203" rel="nofollow">Nevada;</a> </p> <div class="translation"> 机译:古磁石;地磁;逆转;过渡;内科;内华达州; </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/0704023360501.html">Directional change during a <fc >M</fc>M iocene <fc >R</fc>R ‐ <fc >N</fc>N geomagnetic polarity reversal recorded by mafic lava flows, <fc >S</fc>S heep <fc >C</fc>C reek <fc >R</fc>R ange, north central <fc >N</fc>N evada, <fc >USA</fc>USA</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bogue S. 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href="/academic-journal-cn_refrigeration-air-conditioning_thesis/0201286230969.html">非共沸混合工质HFC-32/HFC-125/HFC-134a在家用空调器中替代HCFC-22的实验研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘晓斌&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 刘晓斌</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=蒋能照&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,蒋能照</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=吴兆琳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,吴兆琳</a> <span> <a href="/journal-cn-7719/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 制冷与空调(北京) </a> </span> <span> . 1996</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-28957_thesis/020222108751.html">FCS与后FCS时代</a> <b>[C]</b> <span> <a 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href="/patent-detail/06120104161833.html">浅层电气保护器件(GFCI、AFCI和AFCI/GFCI)系统和方法</a> <b>[P]</b> . <span> 中国专利: CN111492540A </span> <span> . 2020-08-04</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/061201972078.html">PFC信号生成电路、使用PFC信号生成电路的PFC控制系统以及PFC控制方法</a> <b>[P]</b> . <span> 中国专利: CN103503295B </span> <span> . 2016.03.09</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130411183676.html">anschlussvorrichtung to connect an tu00fcrantriebs to a record of a drehflu00fcgeltu00fcr and drehflu00fcgeltu00fcrantrieb and drehflu00fcgeltu00fcr</a> <b>[P]</b> . <span> 外国专利: <!-- 德国专利: --> DE202015000399U1 </span> <span> . 2016-06-02</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:anschlussvorrichtung将t u00fcrantriebs连接到drehfl u00fcgelt u00fcr和drehfl u00fcgelt u00fcrantrieb和drehfl u00fcgelt u00fcr的记录 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130403945924.html">VALVE POSITION SENSOR OF A SLIDING SLEEVE OF A FLOW CONTROLLER VALVE (FCV), FLOW CONTROLLER VALVE (FCV), AND METHOD FOR DETERMINING A POSITION OF A SLIDING SLEEVE OF A FLOW CONTROLLER VALVE (FCV)</a> <b>[P]</b> . <span> 外国专利: <!-- --> BRPI0909741B1 </span> <span> . 2019-06-25</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:流量控制阀的滑套的阀位置传感器,流量控制阀和用于确定流量控制阀的滑套位置的方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130415180468.html">valve position sensor of a flow control valve (fcv) sliding sleeve, flow control valve (fcv), and method for determining a position of a flow control valve (fcv) sliding sleeve</a> <b>[P]</b> . <span> 外国专利: <!-- --> BRPI0909741A2 </span> <span> . 2015-10-06</span> 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