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首页> 外文期刊>Geochemistry, geophysics, geosystems >Emplacement and High‐Temperature Evolution of Gabbros of the 16.5°N Oceanic Core Complexes (Mid‐Atlantic Ridge): Insights Into the Compositional Variability of the Lower Oceanic Crust
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Emplacement and High‐Temperature Evolution of Gabbros of the 16.5°N Oceanic Core Complexes (Mid‐Atlantic Ridge): Insights Into the Compositional Variability of the Lower Oceanic Crust

机译：16.5°N海洋核心复合物（中大西洋山脊）的储层和高温演变：洞察下海外壳的组成变异性

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Abstract >This study reports the composition of the oceanic crust from the 16.5°N region of the Mid‐Atlantic Ridge, a spreading ridge segment characterized by a complex detachment fault system and three main oceanic core complexes (southern, central, and northern OCCs). Lithologies recovered from the core complexes include both greenschist facies and weathered pillow basalt, diabase, peridotite, and gabbro, while only weathered and fresh pillow basalt was dredged from the rift valley floor. The gabbros are compositionally bimodal, with the magmatic crust in the region formed by scattered intrusions of chemically primitive plutonic rocks (i.e., dunites and troctolites), associated with evolved oxide‐bearing gabbros. We use thermodynamic models to infer that this distribution is expected in regions where small gabbroic bodies are intruded into mantle peridotites. The occurrence of ephemeral magma chambers located in the lithospheric mantle enables large proportions of the melt to be erupted after relatively low degrees of fractionation. A large proportion of the dredged gabbros reveal evidence for deformation at high‐temperature conditions. In particular, chemical changes in response to deformation and the occurrence of very high‐temperature ultramylonites (1000?°C) suggest that the deformation related to the oceanic detachment commenced at near‐solidus conditions. This event was likely associated with the expulsion of interstitial, evolved magmas from the crystal mush, a mechanism that enhanced the formation of disconnected oxide‐gabbro seams or layers often associated with crystal‐plastic fabrics in the host gabbros. This granulite‐grade event was soon followed by hydrothermal alteration revealed by the formation of amphibole‐rich veins at high‐temperature conditions (~900?°C). </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> 本研究报告了海底从大西洋脊的16.5°N区的海洋地壳的组成，一种由复杂的分离故障系统和三个主要海洋核心复合物（南部，中央和北方OCH）为特征的传播脊段。 ）。从核心复合物中恢复的岩石包括砂砾派相片和风化的枕头玄武岩，蛋白质，橄榄石和Gabbro，同时只有风化和新鲜的枕头玄武岩从裂谷楼层脱落。 Gabbros是合成的双峰，在由化学原始型岩石（即dunites和塞子）的散射入侵形成的区域中，与进化的氧化物覆盖率相关联的区域形成。我们使用热力学模型来推断，在侵入地幔阶层的小虎斑体内的地区预期这个分布。位于岩石罩中的短颗粒腔的发生能够在相对低的分馏程度之后爆发的大量熔体。大量疏浚的Gabbros揭示了高温条件下变形的证据。特别地，响应变形的化学变化和非常高温尿素（＆ 1000？°C）的发生，表明与海拔有关的变形在近似固体条件下开始。该事件可能与从晶体糊状物中排出的间隙，进化的岩浆驱逐相关，这是一种能够增强与主体Gabbros中的晶体塑料织物的形成的形成的形成的机制。这种粒粒级事件很快，随后通过在高温条件下形成富含阳吡硼的静脉（〜900Ω°C）而揭示的水热改变。</ 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1期</span><b style="margin: 0 2px;">|</b><span>共21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=Sanfilippo A.&option=202" target="_blank" rel="nofollow">Sanfilippo A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dick H. J. B.&option=202" target="_blank" rel="nofollow">Dick H. J. B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marschall H. R.&option=202" target="_blank" rel="nofollow">Marschall H. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lissenberg C. J.&option=202" target="_blank" rel="nofollow">Lissenberg C. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Urann B.&option=202" target="_blank" rel="nofollow">Urann 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>Dipartimento di Scienze della Terra e dell'AmbienteUniversità degli Studi di PaviaPavia Italy;</p> <p>Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>School of Earth and Ocean SciencesCardiff UniversityCardiff UK;</p> <p>Department of Geology and GeophysicsWoods Hole Oceanographic InstitutionWoods Hole MA 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=gabbro&option=203" rel="nofollow">gabbro;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=detachment&option=203" rel="nofollow">detachment;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic core complex&option=203" rel="nofollow">oceanic core complex;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=melt‐rock reactions&option=203" rel="nofollow">melt‐rock reactions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lower oceanic crust&option=203" rel="nofollow">lower oceanic crust;</a> </p> <div class="translation"> 机译：Gabbro;脱离;海洋核心复合物;熔融岩体反应;下海外壳; </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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360513.html">Emplacement and High‐Temperature Evolution of Gabbros of the 16.5°N Oceanic Core Complexes (Mid‐Atlantic Ridge): Insights Into the Compositional Variability of the Lower Oceanic Crust</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sanfilippo A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Sanfilippo A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dick H. 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