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Magnetic Mineralogy and Petrophysical Properties of Ultramafic Rocks: Consequences for Crustal Magnetism

机译：超空地岩石的磁性矿物学和岩石物理特性：地壳磁性的后果

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Abstract >Magnetic properties from the Reinfjord Ultramafic Complex, in northern Norway, which formed as part of a deep magmatic conduit system, have been investigated to determine the magnetic signature of ultramafic rocks now exposed at the surface and deeper in the lower crust. The dominant carriers in these ultramafic rocks are a chrome‐spinel with Fe‐rich exsolution blebs and exsolution lamellae of magnetite in clinopyroxene. Except locally, in a fault zone and in discrete small fractures, these rocks show only minor to no alteration. We infer that the magnetic oxides characterized here are representative of pristine magnetic carriers in similar rocks deeper in the crust. These oxides can be stable in lower crustal, possibly upper mantle, depths when temperatures are below the Curie temperature of magnetite, taking into account pressure effects. These ultramafic rocks are candidates for potential sources of long‐wavelength anomalies. </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> >从Reinfjord Ultramafic复合物中的磁性特性，在挪威北部，形成为深岩石管道系统的一部分，已经研究以确定现在暴露在表面上的超微岩石岩石的磁性签名和下部地壳的更深。这些超空地岩石中的主导载体是Clospoceoxene的Fe-Rich exsolution Blebs和Exsolution Lamellae的铬尖晶石。除本地，在故障区和离散的小骨折中，这些岩石仅展示了次要的不改变。我们推断出于此表征的磁性氧化物代表在地壳中的类似岩石中的原始磁性载体。考虑到压力效应，当温度低于静脉温度时，这些氧化物在较低的地壳中，可能是较低的地壳，可能是上部地幔，深度。这些超空地岩石是用于长波长异常的潜在来源的候选者。</ 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4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=Maat Geertje W.&option=202" target="_blank" rel="nofollow">Maat Geertje W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McEnroe Suzanne A.&option=202" target="_blank" rel="nofollow">McEnroe Suzanne A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Church Nathan S.&option=202" target="_blank" rel="nofollow">Church Nathan S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Larsen Rune B.&option=202" target="_blank" rel="nofollow">Larsen Rune B.;</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 Geoscience and PetroleumNorwegian University of Science and TechnologyTrondheim Norway;</p> <p>Department of Geoscience and PetroleumNorwegian University of Science and TechnologyTrondheim Norway;</p> <p>Department of Geoscience and PetroleumNorwegian University of Science and TechnologyTrondheim Norway;</p> <p>Department of Geoscience and PetroleumNorwegian University of Science and TechnologyTrondheim Norway;</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=ultramafic rocks&option=203" rel="nofollow">ultramafic rocks;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rock magnetism&option=203" rel="nofollow">rock magnetism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=chrome spinel&option=203" rel="nofollow">chrome spinel;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal magnetism&option=203" rel="nofollow">crustal magnetism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magnetic anomalies&option=203" rel="nofollow">magnetic anomalies;</a> </p> <div class="translation"> 机译：超岩石;岩石磁性;铬尖晶石;地壳磁化;磁性异常; 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