中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
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
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
DOI10.3390/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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