Magnetism at Depth: A View from an Ancient Continental Subduction and Collision Zone

McEnroe Suzanne A.; Robinson Peter; Church Nathan; Purucker Michael

摘要

Abstract >Recent sophisticated global data compilations and magnetic surveys have been used to investigate the nature of magnetization in the lower crust and upper mantle. Two approaches to constraining magnetizations are developed, providing minimum (0.01 SI) and maximum (0.04 SI) susceptibility estimates, given some assumed thickness (15+ km here). These values are higher than are found in many continental rocks. Are there rocks deeper in the crust or upper mantle that are more magnetic than expected, or are the model assumptions incomplete? What is the magnetic behavior of deep‐crustal and upper mantle rocks, when slightly cooler than the Curie or Néel temperatures of their magnetic minerals, after being exhumed from locations of high‐grade metamorphism at greater depth? Different sets of equilibrium metamorphic minerals can be considered that would form under different conditions. Results on 1,501 samples from the Western Gneiss Region (WGR) Norway, mainly from mafic and ultramafic bodies subducted to depths of 60–200 km and temperatures of 750 up to 950°C at the very highest pressures, show that rocks did not fully equilibrate to the dominant metamorphic‐facies conditions. There is a large variation in petrophysical properties, oxide minerals, and mineral assemblages in WGR samples, though they cannot explain the broad high‐amplitude (deep‐seated) anomalies measured in this region. The presence of magnetite, and exsolved titanohematite and hemoilmenite in samples, shows those magnetic phases are preserved even at eclogite‐facies conditions, in part because complete eclogite‐facies equilibrium was rarely achieved. </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> <P>最近的复杂全球数据编译和磁性调查已经用于研究下地壳和上部地幔中的磁化性质。制定了两个限制磁化的方法，提供了最小（0.01 si）和最大（0.04 si）敏感性估计，给出了一些假定的厚度（此处15到3公里）。这些值高于许多大陆岩石中的发现。在地壳或上部地幔中是否有岩石更宽的磁力比预期更易，或者模型假设不完整？深色外壳和上部地幔岩石的磁力行为是什么，当比其磁性矿物质的居里或Néel温度稍微冷却，从高档变质的位置处挖掘出来？可以认为不同的平衡变质矿物组将在不同的条件下形成。结果来自西方片（WGR）挪威的1,501个样品，主要来自MAFIC和UltramfiC身体，在60-200公里的深度下，750克的温度高达950°C，表明岩石没有完全平衡到主导的变质形态条件。岩石物理性质，氧化物矿物质和WGR样品中的矿物组合具有大的变化，但不能解释该区域测量的广泛的高幅度（深座位）异常。磁铁矿的存在和exsolved titanohematite和血清矿石在样品中，即使在Eclogite-Faceies条件下也会被保存那些磁性相位，部分是因为很少实现完全的Eclogite面部平衡。</ 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>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共25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=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=Robinson Peter&option=202" target="_blank" rel="nofollow">Robinson Peter;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Church Nathan&option=202" target="_blank" rel="nofollow">Church Nathan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Purucker Michael&option=202" target="_blank" rel="nofollow">Purucker Michael;</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 Geoscience and PetroleumNorwegian University of Science and TechnologyTrondheim Norway;</p> <p>Geological Survey of NorwayTrondheim Norway;</p> <p>Institute for Geoscience and PetroleumNorwegian University of Science and TechnologyTrondheim Norway;</p> <p>NASA—Goddard Space Flight CenterGreenbelt MD 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=magnetic anomalies&option=203" rel="nofollow">magnetic anomalies;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SWARM&option=203" rel="nofollow">SWARM;</a> <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=subduction&option=203" rel="nofollow">subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ultrahigh pressure&option=203" rel="nofollow">ultrahigh pressure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rhombohedral oxides&option=203" rel="nofollow">rhombohedral oxides;</a> </p> <div class="translation"> 机译：磁性异常;群;磁铁矿;俯冲;超高压;菱形氧化物; </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/0704023360734.html">Magnetism at Depth: A View from an Ancient Continental Subduction and Collision Zone</a> <b>[J]</b> . <span> <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" 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