气候变化领域集成服务门户(CCPortal): Early Devonian (415–400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana

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DOI	10.1130/B35412.1;
	Early Devonian (415–400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana
	Xin Y.; Li J.; Ratschbacher L.; Zhao G.; Zhang Y.; Dong S.; Xia X.-P.; Yu Y.
发表日期	2020
ISSN	167606
起始页码	2295
结束页码	2317
卷号	132 期号:11
英文摘要	The evolution of the South China continental crust and its linkage to the assembly and rifting of eastern Gondwana are key issues in the understanding of the early Paleozoic evolution of eastern Asia. We report U-Pb zircon ages and geochemical and Lu-Hf isotopic data for the South Fufang and Yingshang granitoids and the Mayuan diabases from the Wuyishan of eastern South China. The zircons yielded U-Pb ages of ca. 414–404 and ca. 409–401 Ma for the granitoids and diabases, respectively. Petrographic and geochemical features indicate that the granitoids are peraluminous A-type granites, expressed by high Ga/A1 ratios and high Zr, Nb, Ce, Y, and rare earth element contents. They show negative zircon εHf(t) values (-15.4 to -5.8), consistent with the derivation from a crustal source. The granitoids likely originated from partial melting of dry granulite residues in the lower crust. The diabases show depletion in Ti, and negative correlations between FeOt and Mg#, and SiO2 and TiO2/FeOt, reflecting clinopyroxene, olivine, and Fe-Ti oxide fractionation. Their negative zircon εHf(t) values (-4.5 to -0.4) indicate an ancient enriched-mantle origin. The diabases likely originated from partial melting of a subcontinental lithospheric mantle. We interpret these A-type granitoids and diabases as post-orogenic, formed during extensional collapse of thickened crust. Their generation indicates that South China experienced crustal extension during the Early Devonian. The extension occurred coevally with global rifting that led to the separation of the continental blocks of eastern Asia from eastern Gondwana, which was associated with the Early Devonian opening of the paleo-Tethys Ocean. © 2020 Geological Society of America
语种	英语
来源期刊	Bulletin of the Geological Society of America
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/184863
作者单位	Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China; Key Laboratory of Paleomagnetism and Tectonic Reconstruction, Ministry of Natural Resources, Beijing, 100081, China; Geologie, Technische Universität Bergakademie Freiberg, Freiberg, 09599, Germany; Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China; State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing, 210093, China; State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, 510640, China
推荐引用方式 GB/T 7714	Xin Y.,Li J.,Ratschbacher L.,等. Early Devonian (415–400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana[J],2020,132(11).
APA	Xin Y..,Li J..,Ratschbacher L..,Zhao G..,Zhang Y..,...&Yu Y..(2020).Early Devonian (415–400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana.Bulletin of the Geological Society of America,132(11).
MLA	Xin Y.,et al."Early Devonian (415–400 Ma) A-type granitoids and diabases in the Wuyishan, eastern Cathaysia: A signal of crustal extension coeval with the separation of South China from Gondwana".Bulletin of the Geological Society of America 132.11(2020).