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DOI10.1029/2023GL106973
Mantle Plume-Lithosphere Interactions Beneath the Emeishan Large Igneous Province
Zhang, Anqi; Guo, Zhen; Afonso, Juan Carlos; Shellnutt, J. Gregory; Yang, Yingjie
发表日期2024
ISSN0094-8276
EISSN1944-8007
起始页码51
结束页码2
卷号51期号:2
英文摘要The formation of large igneous provinces (LIPs) has been widely believed to be linked to mantle plume activity. However, how the plume modifies the overlying lithosphere, particularly its compositional structure, remains uncertain. Here, we characterize the deep thermochemical structure beneath the Emeishan LIP (ELIP), which is a well-known Permian plume-related LIP in China, by taking a multi-observable probabilistic inversion. Our results find a clear correlation between the lithospheric composition with the ELIP's concentric zones. We infer that the fertile feature of the lithospheric mantle in the ELIP's inner zone was caused by the plume-derived fertile magmas which infiltrated into and chemically refertilized the ambient depleted lithosphere. This plume-modified lithospheric compositional structure is likely to be preserved after the plume event, while the present lithospheric thermal structure has been mainly influenced by the subsequent thermal-tectonic activity. Our results improve our understanding of the physicochemical interactions between the lithosphere and ancient plume. Gaining insights into the nature of large igneous provinces (LIPs) helps understand mass extinction and climate change in the past, since the outpouring of large accumulations of igneous rocks associated with LIPs could alter ancient climates and environments. Here, we focus on a well-known plume-related LIP during the Permian in China, Emeishan LIP (ELIP), to construct its deep thermochemical structure based on a multi-observable probabilistic inversion method. Our results suggest that the bulk fertile feature (not depleted by melt extraction) of the lithospheric mantle in the vicinity of the ELIP's inner zone was caused by the plume-derived fertile magmas which infiltrated into the ambient depleted (deficient in minerals extracted by partial melting of the rock) lithospheric mantle and chemically refertilized it by melt-rock interaction. However, the imaged thermal structure shows a large ongoing asthenospheric upwelling and small-scale thermal convection, implying that the present-day lithospheric thickness has been mainly influenced by the subsequent tectonic events. Our results improve the understanding of the physicochemical interactions between the lithosphere and ancient plume and contribute to the knowledge of the nature of LIPs. Image the thermochemical structure beneath the Emeishan Large Igneous Province via novel joint inversionsReveal plume refertilization of the lithosphere beneath the Emeishan Large Igneous Province's inner zoneImage complex mantle circulation patterns beneath the Emeishan Large Igneous Province region
英文关键词Emeishan large igneous province; multi-observable probabilistic inversion; thermochemical structure; mantle plume-modified lithosphere
语种英语
WOS研究方向Geology
WOS类目Geosciences, Multidisciplinary
WOS记录号WOS:001148152600001
来源期刊GEOPHYSICAL RESEARCH LETTERS
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/305822
作者单位Southern University of Science & Technology; Chinese Academy of Sciences; Innovation Academy for Precision Measurement Science & Technology, CAS; Southern University of Science & Technology; University of Twente; National Taiwan Normal University; Southern University of Science & Technology
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GB/T 7714
Zhang, Anqi,Guo, Zhen,Afonso, Juan Carlos,et al. Mantle Plume-Lithosphere Interactions Beneath the Emeishan Large Igneous Province[J],2024,51(2).
APA Zhang, Anqi,Guo, Zhen,Afonso, Juan Carlos,Shellnutt, J. Gregory,&Yang, Yingjie.(2024).Mantle Plume-Lithosphere Interactions Beneath the Emeishan Large Igneous Province.GEOPHYSICAL RESEARCH LETTERS,51(2).
MLA Zhang, Anqi,et al."Mantle Plume-Lithosphere Interactions Beneath the Emeishan Large Igneous Province".GEOPHYSICAL RESEARCH LETTERS 51.2(2024).
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