中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Proterozoic mantle melting recorded by the Re-Os isotopic systematics of ophiolites from the Qilian Orogenic Belt, northwestern China

文献类型:期刊论文

作者Zhao, Jing; Xiao, Qianru; Gao, Yilin; Zuo, Rui; Huang, Luyu; Li, Jie; Long, Xiaoping
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2023
卷号241页码:105479
关键词ZIRCON U-PB NW CHINA ACCRETIONARY BELT TIBETAN PLATEAU SUBDUCTION INITIATION ABYSSAL PERIDOTITES ULTRAMAFIC ROCKS INTRUSIVE ROCKS NORTHERN MARGIN VOLCANIC-ROCKS
ISSN号1367-9120
DOI10.1016/j.jseaes.2022.105479
英文摘要Re-Os isotopes of the mantle-derived ultramafic rocks can provide temporal constraints on the melt extraction of ancient mantle. Here, new geochemistry and Re-Os isotopes of serpentinites from the Minhe ophiolite in the Qilian Orogenic Belt (QOB) are presented. Their geochemical compositions (e.g., abundances of heavy rare earth elements, Al2O3, Yb, Re, and Th/Yb ratio) suggest that protoliths of the serpentinites originated as mantle res-idues. They underwent multiple episodes of melt depletion, leading to a highly refractory nature and high de-grees of partial melting (>18%). Moreover, subchondritic 187Re/188Os (0.0023-0.0399) and 187Os/188Os (0.1135-0.1210) ratios of the serpentinites, and decoupling of the Re-Os systematics and metasomatic proxies (e. g., LOI, Sr, La, and Th/Yb), demonstrate that fluid/melt metasomatism exerted a limited impact on their Re-Os isotopic systematics. Their Re-depletion ages (TRD), varying from 1.22 to 2.21 Ga, are analogues to their Re-Os model ages (TMA, 1.29-2.31 Ga). Therefore, Re-Os isotopic ages recorded by ophiolites in QOB indicate that at least two major melt-extraction episodes occurred in the lithospheric mantle during Proterozoic (1.2-1.6 Ga and 2.0-2.2 Ga). Notably, the 1.2-1.6 Ga mantle melt-depletion event may have a genetic affinity with the 1.1-1.7 Ga crustal growth. Mantle rocks from an ophiolite have a great potential in tracking ancient geological events, such as Precambrian mantle melting.
WOS研究方向Geosciences, Multidisciplinary
语种英语
WOS记录号WOS:000927574000004
源URL[http://ir.gig.ac.cn/handle/344008/80387]  
专题同位素地球化学国家重点实验室
推荐引用方式
GB/T 7714
Zhao, Jing,Xiao, Qianru,Gao, Yilin,et al. Proterozoic mantle melting recorded by the Re-Os isotopic systematics of ophiolites from the Qilian Orogenic Belt, northwestern China[J]. JOURNAL OF ASIAN EARTH SCIENCES,2023,241:105479.
APA Zhao, Jing.,Xiao, Qianru.,Gao, Yilin.,Zuo, Rui.,Huang, Luyu.,...&Long, Xiaoping.(2023).Proterozoic mantle melting recorded by the Re-Os isotopic systematics of ophiolites from the Qilian Orogenic Belt, northwestern China.JOURNAL OF ASIAN EARTH SCIENCES,241,105479.
MLA Zhao, Jing,et al."Proterozoic mantle melting recorded by the Re-Os isotopic systematics of ophiolites from the Qilian Orogenic Belt, northwestern China".JOURNAL OF ASIAN EARTH SCIENCES 241(2023):105479.

入库方式: OAI收割

来源:广州地球化学研究所

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