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首页> 外文期刊>Geochemistry, geophysics, geosystems >Domain State and Temperature Dependence of Pressure Remanent Magnetization in Synthetic Magnetite: Implications for Crustal Remagnetization
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Domain State and Temperature Dependence of Pressure Remanent Magnetization in Synthetic Magnetite: Implications for Crustal Remagnetization

机译：域状态和温度依赖性对合成磁铁矿中的压力再现磁化：晶体退磁的影响

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Abstract > Pressure remanent magnetization (PRM) is acquired when a rock is compressed in the presence of a magnetic field. This process can take place in many different environments from impact and ejection processes in space, to burial and subsequent uplifting of terrestrial rocks. In this study, we systematically study the acquisition of PRM at different pressures and temperatures, using synthetic magnetite in four different grain sizes ranging from nearly single‐domain to purely multidomain. The magnitude of the PRM acquired in a 300 μ <fi>T</fi> field is, within error, independent of the domain state of the sample. We propose that the acquisition of a PRM is mainly driven by the magnetostriction of the magnetic material. We further show that compared to a thermal remanent magnetization, the acquisition of PRM in large multidomain grains can be quite efficient, and may represent a significant component of magnetization in low‐temperature–high‐pressure environments. </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”XML：ID =“GGGE21893-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> > 当岩石在磁场的存在下被压缩时，获得压力剩磁磁化（PRM）。该过程可以在许多不同的环境中从空间中的冲击和喷射过程中进行，以埋葬和随后的陆地岩石振奋。在这项研究中，我们系统地研究了在不同压力和温度下的PRM的采集，在四种不同粒度范围内的合成磁铁矿范围从几乎单一结构域到纯多麦田。在300μm中获得的PRM的大小 <fi> t </ fi> 在错误中，字段在错误中独立于样本的域状态。我们建议采集PRM主要由磁性材料的磁致伸缩驱动。我们进一步表明，与热再现磁化相比，大型多麦草颗粒的PRM的采集可以非常有效，并且可以代表低温高压环境中的磁化的重要组成部分。 </ 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5期</span><b style="margin: 0 2px;">|</b><span>共11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=Volk Michael W.R.&option=202" target="_blank" rel="nofollow">Volk Michael W.R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Feinberg Joshua M.&option=202" target="_blank" rel="nofollow">Feinberg Joshua M.;</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>Institute for Rock Magnetism Department of Earth SciencesUniversity of MinnesotaMinneapolis MN USA;</p> <p>Institute for Rock Magnetism Department of Earth SciencesUniversity of MinnesotaMinneapolis MN 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=magnetite&option=203" rel="nofollow">magnetite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magnetostriction&option=203" rel="nofollow">magnetostriction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pressure&option=203" rel="nofollow">pressure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=pressure remanence&option=203" rel="nofollow">pressure remanence;</a> </p> <div class="translation"> 机译：磁铁矿;磁致伸缩;压力;压力滞留; 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surface temperature equal to the Curie point of magnetite</a> <b>[P]</b> . <span> 外国专利： <!-- 俄罗斯专利： --> RU2001125694A </span> <span> . 2003-07-20</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：确定洋地壳表面温度等于磁铁矿居里点的位置的方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130453262020.html">METHOD, SYSTEM AND DEVICE FOR DETECTING THE GENERATION AND THE SIZE OF TSUNAMI BY OBSERVING AND MEASURING FROM THE SPACE THE TEMPERATURE RISE OR STEAM QUANTITY ON THE SEA SURFACE OF HUNDREDS KM2 IN TENS SECONDS DUE TO HEAT ENERGY RELEASE AS GREAT NUMBER OF STEAM BUBBLE, BECAUSE OF QUICK DEPRESSION OF WATER PRESSURE WHEN ENERGY GIVEN AS UNDERWATER ACOUSTIC WAVE IN SEA WATER FROM SEABED CRUST BY RAISE, COLLAPSE OF THE SEABED CRUST OR ACCELERATED VIBRATION DUE TO EARTHQUAKE WITH EPICENTER AT THE SEABED REACHES THE SEA SURFACE AT 1500 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