中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Ancient Refertilization Process Preserved in the Plagioclase Peridotites: An Example From the Shuanggou Ophiolite, Southwest China

文献类型:期刊论文

作者Hu, Wen-Jun2,3; Zhong, Hong1,2; Chu, Zhu-Yin4; Zhu, Wei-Guang2; Bai, Zhong-Jie2; Zhang, Chang4
刊名JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
出版日期2020
卷号125期号:1页码:21
关键词Shuanggou ophiolite mantle refertilization platinum group elements Re-Os isotopes
ISSN号2169-9313
DOI10.1029/2019JB017552
英文摘要Petrology, geochemistry, platinum group elements (PGEs: Os, Ir, Ru, Rh, Pt, and Pd), and Re-Os isotope data of harzburgites and plagioclase lherzolites from the Shuanggou ophiolite (southwest China) are presented in this study, in order to determine whether ancient refertilization process can be preserved in ophiolitic plagioclase peridotites. The harzburgites in the Shuanggou ophiolite are divided into two groups: (1) the Group-1 harzburgites have Os-187/Os-188 ratios (0.12297-0.12727) and PGE abundances similar to those of oceanic peridotites, thereby representing the convecting upper mantle; (2) the Group-2 harzburgites have extremely low Os-187/Os-188 ratios (0.11307-0.11651) with considerable fractionation in iridium group PGEs (Os, Ir, and Ru), indicative of an ancient refractory mantle in the oceanic lithosphere. The plagioclase lherzolites were formed by melt impregnation of the Group-2 harzburgites, according to the PGE compositions and the petrographic features. However, the large Os isotope difference between the lherzolites (Os-187/Os-188: 0.12470-0.12666) and the Group-2 harzburgites indicates that the refertilization process took place much earlier than the exhumation of the mantle at 0.4 Ga. In addition, clinopyroxene composition suggests that the percolating melt is different from the Shuanggou diabases and typical mid-ocean ridge basalts. This study therefore demonstrates that some plagioclase lherzolites possibly were not related to mantle exhumation beneath the spreading center but formed by much older melt impregnation processes in the mantle instead.
WOS关键词PLATINUM-GROUP ELEMENTS ; HIGHLY SIDEROPHILE ELEMENTS ; RE-OS ISOTOPES ; LITHOSPHERIC MANTLE BENEATH ; ARC/BACK-ARC ASSEMBLAGES ; PLATE TECTONIC CYCLE ; PALEO-TETHYS OROGEN ; RIVER SHEAR ZONE ; ABYSSAL PERIDOTITES ; SIBERIAN CRATON
资助项目National Natural Science Foundation of China[41425011] ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences[XDB18000000]
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000530895100007
出版者AMER GEOPHYSICAL UNION
资助机构National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; National Natural Science Foundation of China ; National Natural Science Foundation of China ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences ; Strategic Priority Research Program (B) of the Chinese Academy of Sciences
源URL[http://ir.iggcas.ac.cn/handle/132A11/96724]  
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Zhong, Hong
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geochem, State Key Lab Ore Deposit Geochem, Guiyang, Peoples R China
3.Univ Hong Kong, Dept Earth Sci, Hong Kong, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing, Peoples R China
推荐引用方式
GB/T 7714
Hu, Wen-Jun,Zhong, Hong,Chu, Zhu-Yin,et al. Ancient Refertilization Process Preserved in the Plagioclase Peridotites: An Example From the Shuanggou Ophiolite, Southwest China[J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,2020,125(1):21.
APA Hu, Wen-Jun,Zhong, Hong,Chu, Zhu-Yin,Zhu, Wei-Guang,Bai, Zhong-Jie,&Zhang, Chang.(2020).Ancient Refertilization Process Preserved in the Plagioclase Peridotites: An Example From the Shuanggou Ophiolite, Southwest China.JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH,125(1),21.
MLA Hu, Wen-Jun,et al."Ancient Refertilization Process Preserved in the Plagioclase Peridotites: An Example From the Shuanggou Ophiolite, Southwest China".JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH 125.1(2020):21.

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来源:地质与地球物理研究所

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