Subduction-Induced Fractionated Highly Siderophile Element Patterns in Forearc Mantle
文献类型:期刊论文
作者 | Xu, Yang1,2,3; Liu, Chuan-Zhou1,2,3,4 |
刊名 | MINERALS
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出版日期 | 2019-06-01 |
卷号 | 9期号:6页码:17 |
关键词 | highly siderophile elements (HSEs) subduction zones forearc mantle New Caledonia ophiolites |
ISSN号 | 2075-163X |
DOI | 10.3390/min9060339 |
英文摘要 | Compositions of highly siderophile elements (HSEs) in forearc mantle have been little studied and effects of slab dehydration on their abundances in forearc mantle remains unclear. This study reports two different kinds of HSE patterns for peridotites from a New Caledonia forearc ophiolite. The Group-I samples show relatively flat patterns of Ir-group-platinum-group elements (IPGEs) and enrichment of Pt over Pd. Such patterns imply that interstitial sulfides were significantly removed through melt extraction, whereas sulfides enclosed within silicates were mostly unaffected. Meanwhile, Pt-Fe alloys were generated, resulting in suprachondritic Pt/Pd ratios. In contrast, the Group-II samples display convex HSE patterns and are depleted in all HSEs except for Ru, yielding strongly positive Ru anomalies. This indicates that both enclosed and interstitial sulfides were substantially consumed, whereas chromite was generated to stabilize Ru. Compared to abyssal peridotites, subduction-related peridotites commonly have stronger fractionation in the HSEs. Therefore, the HSE data of mantle peridotites are potentially able to discriminate the tectonic settings of ophiolites. |
WOS关键词 | SHETLAND OPHIOLITE COMPLEX ; PLATINUM-GROUP ELEMENTS ; NEW-CALEDONIA ; OS ISOTOPE ; PERIDOTITE XENOLITHS ; ABYSSAL PERIDOTITES ; SOUTHWEST PACIFIC ; MELT PERCOLATION ; OMAN OPHIOLITE ; SUD OPHIOLITE |
资助项目 | National Natural Science Foundation of China[41673038] ; Key Research Program of Frontier Sciences[QYZDB-SSW-DQC032] ; Chinese Academy of Sciences ; National Key R&D Program of China[2016YFE0203000] |
WOS研究方向 | Mineralogy ; Mining & Mineral Processing |
语种 | 英语 |
WOS记录号 | WOS:000473809300012 |
出版者 | MDPI |
资助机构 | National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Key Research Program of Frontier Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; Chinese Academy of Sciences ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/92689] ![]() |
专题 | 地质与地球物理研究所_岩石圈演化国家重点实验室 |
通讯作者 | Liu, Chuan-Zhou |
作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Shandong, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 4.CAS Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China |
推荐引用方式 GB/T 7714 | Xu, Yang,Liu, Chuan-Zhou. Subduction-Induced Fractionated Highly Siderophile Element Patterns in Forearc Mantle[J]. MINERALS,2019,9(6):17. |
APA | Xu, Yang,&Liu, Chuan-Zhou.(2019).Subduction-Induced Fractionated Highly Siderophile Element Patterns in Forearc Mantle.MINERALS,9(6),17. |
MLA | Xu, Yang,et al."Subduction-Induced Fractionated Highly Siderophile Element Patterns in Forearc Mantle".MINERALS 9.6(2019):17. |
入库方式: OAI收割
来源:地质与地球物理研究所
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