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Oxygen fugacity evolution of the mantle lithosphere beneath the North China Craton
Ye, Chen-Yang1,2; Ying, Ji-Feng1,2,3; Tang, Yan-Jie1,2,3; Zhao, Xin-Miao1,3; Zhang, Hong-Fu1,2
2021-12-19
Source PublicationINTERNATIONAL GEOLOGY REVIEW
ISSN0020-6814
Pages16
AbstractOxygen 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.
KeywordOxygen fugacity peridotite lithospheric mantle metasomatism North China Craton
DOI10.1080/00206814.2021.2015630
Funding OrganizationNational 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
WOS KeywordSINO-KOREAN CRATON ; PERIDOTITE XENOLITHS ; OXIDATION-STATE ; SHANDONG PROVINCE ; TRACE-ELEMENT ; FERRIC IRON ; OS ISOTOPES ; TEMPORAL EVOLUTION ; MELT PERCOLATION ; WATER CONTENTS
Language英语
Funding ProjectNational Natural Science Foundation of China[41688103] ; National Natural Science Foundation of China[41725014]
Funding OrganizationNational 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
WOS Research AreaGeology
WOS SubjectGeology
WOS IDWOS:000731890600001
PublisherTAYLOR & FRANCIS INC
Citation statistics
Document Type期刊论文
Identifierhttp://ir.iggcas.ac.cn/handle/132A11/103903
Collection岩石圈演化国家重点实验室
Corresponding AuthorYing, Ji-Feng
Affiliation1.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing, Peoples R China
3.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing, Peoples R China
First Author AffilicationState Key Laboratory of Lithospheric Evolution
Corresponding Author AffilicationState Key Laboratory of Lithospheric Evolution
Recommended Citation
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.
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