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  4. 岩石圈演化国家重点实验室
Oxygen fugacity evolution of the mantle lithosphere beneath the North China Craton

文献类型：期刊论文

作者Ye, Chen-Yang1,2; Ying, Ji-Feng1,2,3; Tang, Yan-Jie1,2,3; Zhao, Xin-Miao2,3; Zhang, Hong-Fu1,2
刊名INTERNATIONAL GEOLOGY REVIEW
出版日期2021-12-19
页码16
关键词Oxygen fugacity peridotite lithospheric mantle metasomatism North China Craton
ISSN号0020-6814
DOI10.1080/00206814.2021.2015630
英文摘要Oxygen fugacity controls the behaviour of multivalent elements and compositions of C-O-H fluids in Earth's mantle, which further affects the cycling of materials between the deep interior and surface of Earth. The redox state of the mantle lithosphere of typical stable cratons has been well documented, but how oxygen fugacity had varied during craton destruction remains unclear. This study estimates the oxygen fugacity of peridotite xenoliths entrained in Mesozoic and Cenozoic basalts on North China Craton (NCC), a typical destroyed craton. The oxygen fugacity vs. Mg# of olivine reveals that the mantle lithosphere beneath the NCC experienced three stages of evolution in terms of oxygen fugacity. First, the refractory and oxidized peridotite xenoliths indicate that the lithospheric mantle experienced a high degree of melt extraction and later long-term and complicated metasomatism before craton destruction. Then, the variations of olivine Mg-number in peridotites and oxygen fugacity reveal significant metasomatism by melts originated from the shallow asthenosphere during the destruction of the NCC since the Mesozoic. The third stage may have occurred when mantle peridotites interacted with silica-undersaturated melts or fluids stemmed from the mantle transition zone where the stagnant Pacific slab underlies. This study further verifies that the asthenospheric convection induced by the roll-back of the subducted paleo-Pacific slab played a crucial role in the destruction of the NCC and helps understand the oxygen fugacity variability during the later life of the craton.
WOS关键词SINO-KOREAN CRATON ; PERIDOTITE XENOLITHS ; OXIDATION-STATE ; SHANDONG PROVINCE ; TRACE-ELEMENT ; FERRIC IRON ; OS ISOTOPES ; TEMPORAL EVOLUTION ; MELT PERCOLATION ; WATER CONTENTS
资助项目National Natural Science Foundation of China[41688103] ; National Natural Science Foundation of China[41725014]
WOS研究方向Geology
语种英语
WOS记录号WOS:000731890600001
出版者TAYLOR & FRANCIS INC
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 ; National Natural Science Foundation 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 ; National Natural Science Foundation 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 ; National Natural Science Foundation of China ; National Natural Science Foundation of China
源URL[http://ir.iggcas.ac.cn/handle/132A11/103903]  
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Ying, Ji-Feng
作者单位1.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Ye, Chen-Yang,Ying, Ji-Feng,Tang, Yan-Jie,et al. Oxygen fugacity evolution of the mantle lithosphere beneath the North China Craton[J]. INTERNATIONAL GEOLOGY REVIEW,2021:16.
APA Ye, Chen-Yang,Ying, Ji-Feng,Tang, Yan-Jie,Zhao, Xin-Miao,&Zhang, Hong-Fu.(2021).Oxygen fugacity evolution of the mantle lithosphere beneath the North China Craton.INTERNATIONAL GEOLOGY REVIEW,16.
MLA Ye, Chen-Yang,et al."Oxygen fugacity evolution of the mantle lithosphere beneath the North China Craton".INTERNATIONAL GEOLOGY REVIEW (2021):16.

入库方式： OAI收割

来源：地质与地球物理研究所

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