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Water and Oxygen Fugacity in the Lithospheric Mantle Wedge beneath the Northern Canadian Cordillera (Alligator Lake)

机译：北加拿大科特勒拉（鳄鱼湖）下面的岩石架楔形水和氧气污垢

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Abstract >Assessing water contents of subduction zone mantle peridotites can gain insight into the compositions of slab‐derived fluids/melts and the active margin water cycle. Here eight mantle xenoliths from Alligator Lake (northern Canadian Cordillera) are examined to address these issues. The harzburgites have less water, on average, but are more oxidized (ΔFMQ?~?0.1) than the lherzolites (ΔFMQ?~??1.0). The lherzolites have major and trace element compositions close to primitive mantle, while the harzburgite major element and heavy rare earth element compositions are indicative of higher degrees of melt depletion but with light rare earth element‐enriched profiles. Correlations between lherzolite pyroxene water contents and bulk rock Ba/Nb and Ba/Yb ratios likely result from interaction with subduction related fluids. The trace element compositions of the harzburgite clinopyroxenes are successfully modeled by melting of a fertile mantle lithosphere and interaction with a carbonatite melt. Correlations between the harzburgite water contents and clinopyroxene Ca/Al ratios and Mg# are also consistent with the influence of carbonatite metasomatism. Metasomatism likely resulted from opening of a slab window beneath the region, detected as a low‐velocity seismic anomaly, which heated and mobilized a heterogeneous mantle lithosphere veined with carbonatite. This study confirms that subduction zone mantle lithosphere is not necessarily more water‐rich or more oxidized than oceanic lithosphere or other off‐cratonic settings. Moreover, local oxidation is not necessarily related to the ingress of subduction zone fluids but can also be related to melting of a heterogeneous lithosphere following heating above a slab window. </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> >评估俯冲区的水含量披膜偏见可以深入了解板衍生的流体/熔体的组合物和主动边缘水循环。在这里，八个来自鳄鱼湖（北加拿大Cordillera）的搭桥Xenoliths审查了这些问题。 Harzburgites平均水的水较少，但比Lherzolites（Δfmq？~~~1.10）更氧化（Δfmq？0.1）。 Lherzolites具有靠近原始地幔的主要和痕量元素组合物，而Harzburgite主要元素和重质稀土元素组合物表示较高的熔体耗竭，但具有轻质稀土元素的富含型材。 LorzoLite辉石水含量与散岩BA / Nb和Ba / Yb比率之间的相关性可能是与俯冲相关流体的相互作用导致的。通过肥沃的地幔岩石圈融化和与碳酸石熔体相互作用，成功建模了哈尔茨堡钛矿冠状藻酸的痕量元素组合物。 Harzburgite水含量和Clinococoxene Ca / Al比和Mg＃之间的相关性也与碳酸石矿石弥言的影响一致。弥伸主义可能是由在区域下方的平板窗口打开，被检测为低速地震异常，其加热和动员具有碳酸石的异质地幔岩石圈。本研究证实，俯冲区岩石圈不一定比海洋岩石圈或其他脱裂性设置更多的水富含水或更氧化。此外，局部氧化不一定与俯冲区流体的入口有关，但也可以与在平板窗口上方加热后的异质岩石圈的熔化有关。</ 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10期</span><b style="margin: 0 2px;">|</b><span>共26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=Kilgore McKensie L.&option=202" target="_blank" rel="nofollow">Kilgore McKensie L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peslier Anne H.&option=202" target="_blank" rel="nofollow">Peslier Anne H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Brandon Alan D.&option=202" target="_blank" rel="nofollow">Brandon Alan D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lamb William M.&option=202" target="_blank" rel="nofollow">Lamb William 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>Department of Earth and Atmospheric SciencesUniversity of HoustonHouston TX USA;</p> <p>Jacobs Mail Code XI3 Astromaterials Research and Exploration ScienceNASA‐Johnson Space CenterHouston TX USA;</p> <p>Department of Earth and Atmospheric SciencesUniversity of HoustonHouston TX USA;</p> <p>Department of Geology and GeophysicsTexas A&</p> <p>M UniversityCollege Station TX 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=mantle water&option=203" rel="nofollow">mantle water;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=FTIR&option=203" rel="nofollow">FTIR;</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=slab window&option=203" rel="nofollow">slab window;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Canadian Cordillera&option=203" rel="nofollow">Canadian Cordillera;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=metasomatism&option=203" rel="nofollow">metasomatism;</a> </p> <div class="translation"> 机译：地幔;ftir;俯冲;平板窗口;加拿大科特勒拉;弥撒; 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<b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120202008807.html">拉边机水包胶管防折支撑架</a> <b>[P]</b> . <span> 中国专利： CN202011830U </span> <span> . 2011.10.19</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130474263039.html">APPARATUS FOR EXTRACTING ENERGY FROM THE MOTION OF WATER BENEATH WAVES IN A LARGE BODY OF WATER SUCH AS AN OCEAN OR A LAKE</a> <b>[P]</b> . <span> 外国专利：  IN152925B </span> <span> . 1984-05-05</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：从诸如海洋或湖泊的大水中的波浪中的水的运动中提取能量的装置 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130483801915.html">Oxygen supply unit for use in oxygen-deficient waters - e.g. lakes, rivers, etc.</a> <b>[P]</b> . <span> 外国专利：  DE2416773A1 </span> <span> . 1975-10-09</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：供缺氧水中使用的氧气供应装置-例如湖泊，河流等 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130433617223.html">METHOD FOR ELIMINATING OXYGEN-POOR WATER AREA IN DAM LAKE, LAKE, MARSH OR THE LIKE</a> <b>[P]</b> . <span> 外国专利：  JP2008100176A </span> <span> . 2008-05-01</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：消除大湖，湖泊，沼泽或类似湖泊中缺氧水域的方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" 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