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Lithospheric Architecture and Mantle Metasomatism Linked to Iron Oxide Cu‐Au Ore Formation: Multidisciplinary Evidence from the Olympic Dam Region, South Australia

机译：与氧化铁Cu-Au Ou矿石形成有关的岩石树立架构和地幔弥扑结构：来自南澳大利亚奥林匹克坝区的多学科证据

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Abstract >The role of lithospheric architecture and the mantle in the genesis of iron oxide copper‐gold (IOCG) deposits is controversial. Using the example of the Precambrian Gawler Craton (South Australia), which hosts the giant Olympic Dam IOCG deposit, we integrate geophysical data (seismic tomography and magnetotellurics) with geological and geochemical data to develop a new interpretation of the lithospheric setting of these deposits. Spatially, IOCG deposits are located above the margin of a mantle lithospheric zone with anomalously high electrical conductivities (resistivity 10?ohm.m, top at ~100–150?km depth), low seismic shear‐wave velocities (horizontal component, Vsh??4.6?km/s), and unusually high ratios of compressional‐ to shear‐wave velocities (Vp/Vsh??1.80). The high conductivity cannot be explained by water‐bearing olivine‐rich rock alone. Relatively fertile and metasomatized peridotitic mantle with additional high‐Vp/Vs phases, for example, clinohumite, hydrous garnet, and/or phlogopite, could explain the anomalous velocity and conductivity. The top of this high‐Vp/Vsh zone marks a midlithospheric discontinuity at ~100–130?km depth that is interpreted to reflect locally orthopyroxene‐rich mantle. A sub‐Moho zone with high Vp/Vsh at ~40–80?km depth correlates spatially with primitive Nd isotope signatures and arc‐related ~1,620–1,610?Ma magmatism and is interpreted as the eclogitic root of a magmatic arc. Mafic volcanics contemporaneous with ~1,590?Ma IOCG mineralization have geochemistry suggesting derivation from subduction‐modified lithospheric mantle. We suggest that Olympic Dam formed inboard of a continental margin in a postsubduction setting, related to foundering of previously refertilized and metasomatized lithospheric mantle. Deposits formed during the switch from compression to extension, following delamination‐related uplift and exhumation. </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> >岩石结构建筑的作用与氧化铁铜金（IoCG）沉积物的成因中的作用是有争议的。利用托管巨型奥林匹克国际大坝IoCG存款的前宣布吉拉德勒·克拉顿（南澳大利亚）的例子，我们将地球物理数据（地震断层扫描和磁音）与地质和地球化学数据集成，以开发对这些矿床的岩石树形设置的新解释。空间上，IOCG沉积物以异常高电导率（电阻率<ohm，顶部〜100-150Ω·km深度），地震剪切波速度（水平部件， vsh？＆？4.6？km / s），对剪切波速度的异常高比率（vp / vsh？＆？1.80）。单独的含水橄榄石的岩石不能解释高电导率。具有额外的高VP / VS相的相对肥沃和偏偏的偏心型搭桥，例如Clinohumite，含水石榴石和/或植物，可以解释异常的速度和导电性。这种高VP / VSH区的顶部标志着〜100-130的中型性不连续性，被解释为反射众多富含卵状的富含碎屑的地幔。具有高VP / VSH的子Moho区，在〜40-80？km深度与原始Nd同位素签名和电弧相关的〜1,620-1,610？ma magmatism，并被解释为岩晶弧的eClogitic根。 MAFIC火山中的同时〜1,590？MA IOCG矿化有地球化学暗示俯冲改性岩石罩的推导。我们建议奥林匹克大坝在邮政建设中形成欧陆边缘，与先前引用的和弥赛化的岩石树木罩的创始有关。在切换过程中形成的沉积物从压制到延伸，后续分层相关的隆起和挖掘。</ 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8期</span><b style="margin: 0 2px;">|</b><span>共33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=Skirrow R. G.&option=202" target="_blank" rel="nofollow">Skirrow R. G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wielen S. E.&option=202" target="_blank" rel="nofollow">Wielen S. E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Champion D. C.&option=202" target="_blank" rel="nofollow">Champion D. C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Czarnota K.&option=202" target="_blank" rel="nofollow">Czarnota K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Thiel S.&option=202" target="_blank" rel="nofollow">Thiel S.;</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>Geoscience AustraliaCanberra ACT Australia;</p> <p>Geoscience AustraliaCanberra ACT Australia;</p> <p>Geoscience AustraliaCanberra ACT Australia;</p> <p>Geoscience AustraliaCanberra ACT Australia;</p> <p>Geological Survey of South AustraliaAdelaide South Australia Australia;</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=lithospheric architecture&option=203" rel="nofollow">lithospheric architecture;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gawler Craton&option=203" rel="nofollow">Gawler Craton;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Olympic Dam deposit&option=203" rel="nofollow">Olympic Dam deposit;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=IOCG deposits&option=203" rel="nofollow">IOCG deposits;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle metasomatism&option=203" rel="nofollow">mantle metasomatism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tectonic setting&option=203" rel="nofollow">tectonic setting;</a> </p> <div class="translation"> 机译：岩石架构;Gawler Craton;奥林匹克坝床;IOCG沉积物;地幔弥扑术;构造环境; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360496.html">Lithospheric Architecture and Mantle Metasomatism Linked to Iron Oxide Cu‐Au Ore Formation: Multidisciplinary Evidence from the Olympic Dam Region, South Australia</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Skirrow R. 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