Origin of arc-like intraplate volcanism by melting of lithospheric mantle pyroxenite of the South China continental margin

doi:10.1016/j.lithos.2021.106236

IOCAS-IR > 海洋地质与环境重点实验室

	Origin of arc-like intraplate volcanism by melting of lithospheric mantle pyroxenite of the South China continental margin
	Zhao, Zhi-Hua1,2,3,4 ; Zhang, Guo-Liang 1,2,3; Wang, Shuai 1,2,3,4; Zhao, Jian-Xin 5
	2021-09-01
发表期刊	LITHOS
ISSN	0024-4937
卷号	396 页码:10
通讯作者	Zhang, Guo-Liang([email protected])
摘要	Volcanic arcs usually produce silica-rich magmas that may modify the peridotitic sub-arc mantle, but direct observations on the lithology and geochemistry of the sub-arc lithospheric mantle are rare. An Andean-type arc system is inferred on the continental margin of southeastern China during the Mesozoic time; however, direct petrologic evidence for such an ancient arc is lacking. In this study, we have analyzed whole-rock major and trace elements, Sr-Nd-Pb-Hf isotope, and high-precision olivine geochemistry of the basaltic rocks of the Leizhou Peninsula and Hainan Island, on the South China continental margin. Unlike Hainan Island with only typical ocean island basalt (OIB)-type basalts, the Leizhou Peninsula has volcanic rocks ranging from typical OIB-type basalts to island arc basalt (IAB)-type with enrichment in large-ion lithophile elements and depletion in high-field-strength elements. The IAB-like rocks of the Leizhou Peninsula have less radiogenic Nd and Hf isotopes than the Hainan OIB-type basalts and the sub-continental lithospheric mantle. The IAB-like rocks can be explained by interaction of the Hainan plume with a subduction-derived component based on the plots of Nb/Nb* vs. Ce/Pb, Ba/Nb, Pb/Pb*, and SiO2. Olivine phenocrysts with anomalously high Ni and low Ca and Mn contents are consistent with a pyroxenite-rich mantle source for the IAB-like rocks. We suggest that the pyroxenite-rich mantle component of the IAB-like rocks formed by metasomatic reaction between silica-rich arc melts and the sub-continental lithospheric mantle during an ancient plate subduction event. We suggest that these arc-like volcanic rocks record melting of lithospheric mantle pyroxenite triggered by the Hainan plume. Our results are consistent with an Andean-type active continental margin related to subduction of the paleo-Pacific Plate beneath the southeastern China during the Mesozoic. (C) 2021 Elsevier B.V. All rights reserved.
关键词	Metasomatism Lithospheric mantle Pyroxenite Plate subduction Hainan plume South China
DOI	10.1016/j.lithos.2021.106236
收录类别	SCI
语种	英语
资助项目	Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42020302]; Strategic Priority Research Program of the Chinese Academy of Sciences[XDA22050101]; National Natural Science Foundation of China[41876040]; National Natural Science Foundation of China[91858206]; Taishan Scholars Program of Shandong Province[tsqn201909157]; Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology[MGQNLM-TD201806]
WOS研究方向	Geochemistry & Geophysics ; Mineralogy
WOS类目	Geochemistry & Geophysics ; Mineralogy
WOS记录号	WOS:000670299200002
出版者	ELSEVIER
引用统计	被引频次：10[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/177024
专题	海洋地质与环境重点实验室
通讯作者	Zhang, Guo-Liang
作者单位	1.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao 266071, Peoples R China 2.Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China 3.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China 4.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 5.Univ Queensland, Sch Earth & Environm Sci, Radiogen Isotope Facil, Brisbane, Qld 4072, Australia
第一作者单位	中国科学院海洋研究所
通讯作者单位	中国科学院海洋研究所
推荐引用方式 GB/T 7714	Zhao, Zhi-Hua,Zhang, Guo-Liang,Wang, Shuai,et al. Origin of arc-like intraplate volcanism by melting of lithospheric mantle pyroxenite of the South China continental margin[J]. LITHOS,2021,396:10.
APA	Zhao, Zhi-Hua,Zhang, Guo-Liang,Wang, Shuai,&Zhao, Jian-Xin.(2021).Origin of arc-like intraplate volcanism by melting of lithospheric mantle pyroxenite of the South China continental margin.LITHOS,396,10.
MLA	Zhao, Zhi-Hua,et al."Origin of arc-like intraplate volcanism by melting of lithospheric mantle pyroxenite of the South China continental margin".LITHOS 396(2021):10.

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