Geochemical and lead isotope compositions of olivine-hosted melt inclusions from the Yaeyama Graben in the southern Okinawa Trough: Implications for slab subduction and magmatic processes

doi:10.1016/j.lithos.2021.106263

CORC > 海洋研究所 > 中国科学院海洋研究所 > 海洋地质与环境重点实验室

	Geochemical and lead isotope compositions of olivine-hosted melt inclusions from the Yaeyama Graben in the southern Okinawa Trough: Implications for slab subduction and magmatic processes
	Li, Xiaohui 1,4,5; Ren, Zhongyuan 3; Li, Sanzhong 1,4; Zeng, Zhigang 4,5; Yang, Huixin 1; Zhang, Le 3; Guo, Kun 2; Wang, Xiaoyuan 4,5
刊名	LITHOS
	2021-10-01
卷号	398 页码:14
关键词	Melt inclusions Lead isotope Petrogenesis Heterogeneous magma source Okinawa Trough Western Pacific
ISSN号	0024-4937
DOI	10.1016/j.lithos.2021.106263
通讯作者	Li, Xiaohui(xiaohuili@ouc.edu.cn)
英文摘要	Chemical compositions were measured in olivine-hosted melt inclusions in basaltic volcanic rocks from the Yaeyama Graben in the southern Okinawa Trough to investigate the magmatic processes of erupted lavas in an incipient epicontinental back-arc basin in the western Pacific. Melt inclusions have widely variable element and Pb isotope compositions, while erupted host whole-rock compositions are homogeneous, suggesting that melt inclusions preserve more information about magmatic processes than their host whole rocks. Two groups of melt inclusions can be distinguished by their trace elements and Pb isotopes. Group 1 melt inclusions have geochemical compositions similar to those of their host whole rocks, which have low Pb-207/Pb-206 ratios (<0.850), and may be attributed to the contributions of recycled continental crust and subducted sediments to magma sources during Philippine Sea Plate subduction. Group 2 melt inclusions have higher Pb-207/Pb-206 ratios (>0.850) and Li, Rb, and U contents and lower Cu, Zn, and Pb contents than their host whole rocks. High Li, Rb, and U contents may be induced by specific melts generated by possible breakdown reactions of some accessory minerals, such as phengite and cordierite, while low Cu, Zn, and Pb contents are attributed to sulfide precipitation, metal flushing and/or metallic element fractionation during magma evolution. The Pb isotopes of the group 2 melt inclusions are similar to those of the Kuanhsi-Chutung basalts, which are correlated with some intraplate volcanism in the Fujian-Taiwan region. We infer that the group 2 melts were preexisting small volumes of magma that were emplaced in the middle-lower continental crust (similar to 11 km), experienced extensive magma evolution and were entrained by upwelling magma. Our melt inclusion data suggest that magma sources are compositionally heterogeneous and that the mixing of magmas from different sources may be widespread beneath the southern Okinawa Trough because of Philippine Sea Plate subduction and preexisting intraplate magmatism.
资助项目	National Natural Science Foundation of China[42006052] ; National Natural Science Foundation of China[91958214] ; Chinese Academy of Science[XDB42020402] ; China Postdoctoral Science Foundation[2020M672018] ; Shandong Provincial Natural Science Foundation, China[ZR2020MD068] ; Open Fund of the Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences[MGE2019KG07] ; Qingdao Postdoctoral Applied Research Project
WOS研究方向	Geochemistry & Geophysics ; Mineralogy
语种	英语
出版者	ELSEVIER
WOS记录号	WOS:000687292900004
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/176287]
专题	海洋研究所_海洋地质与环境重点实验室
通讯作者	Li, Xiaohui
作者单位	1.Ocean Univ China, Coll Marine Geosci, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Key Lab Submarine Geosci & Prospecting Tech,MOE, Qingdao 266100, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Ctr Isotope Geochem & Geochronol, Qingdao 266237, Peoples R China 3.Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Isotope Geochem, Guangzhou 510640, Peoples R China 4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China 5.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
推荐引用方式 GB/T 7714	Li, Xiaohui,Ren, Zhongyuan,Li, Sanzhong,et al. Geochemical and lead isotope compositions of olivine-hosted melt inclusions from the Yaeyama Graben in the southern Okinawa Trough: Implications for slab subduction and magmatic processes[J]. LITHOS,2021,398:14.
APA	Li, Xiaohui.,Ren, Zhongyuan.,Li, Sanzhong.,Zeng, Zhigang.,Yang, Huixin.,...&Wang, Xiaoyuan.(2021).Geochemical and lead isotope compositions of olivine-hosted melt inclusions from the Yaeyama Graben in the southern Okinawa Trough: Implications for slab subduction and magmatic processes.LITHOS,398,14.
MLA	Li, Xiaohui,et al."Geochemical and lead isotope compositions of olivine-hosted melt inclusions from the Yaeyama Graben in the southern Okinawa Trough: Implications for slab subduction and magmatic processes".LITHOS 398(2021):14.