An Early Cretaceous carbonate replacement origin for the Xinqiao stratabound massive sulfide deposit, Middle-Lower Yangtze Metallogenic Belt, China

doi:10.1016/j.oregeorev.2016.08.017

CORC > 地质与地球物理研究所 > 中国科学院地质与地球物理研究所 > 岩石圈演化国家重点实验室

	An Early Cretaceous carbonate replacement origin for the Xinqiao stratabound massive sulfide deposit, Middle-Lower Yangtze Metallogenic Belt, China
	Li, Yang 1,2; Li, Jian-Wei 5; Li, Xian-Hua 3; Selby, David 2; Huang, Guang-Huan 1; Chen, Lin-Jie 4; Zheng, Kai 4
刊名	ORE GEOLOGY REVIEWS
	2017
卷号	80 页码:985-1003
关键词	Stratabound massive sulfide deposit SIMS oxygen isotope Zircon U-Pb Pyrite Re-Os Fluid inclusion Carbonate replacement deposit
DOI	10.1016/j.oregeorev.2016.08.017
文献子类	Article
英文摘要	Stratabound massive sulfide deposits are widespread along the Middle-Lower Yangtze Metallogenic Belt (MLYMB) and serve as an important copper producer in China. Two contrasting genetic models have been proposed, interpreting the stratabound massive sulfide deposits as a Carboniferous SEDEX protore overprinted by Cretaceous magmatic-hydrothermal system or an Early Cretaceous carbonate replacement deposit. These two contrasting models have been applied to the Xinqiao stratabound Cu-Au sulfide deposit, which is dominated by massive sulfide ores hosted in marine carbonates of the Carboniferous Chuanshan and Huanglong Formations, with minor Cu-Au skarn ores localized in the contact zone between the Cretaceous diorite Jitou stock and the Carboniferous carbonate rocks. New SIMS zircon U-Pb dating suggests that the Jitou stock formed at 138.5 +/- 1.1 Ma (2 sigma, MSWD = 0.6). Pyrite Re-Os dating yields an imprecise date of 142 +/- 47 Ma (2 sigma, MSWD = 7.8). The geochronological data thus constrain the mineralization of the Xinqiao deposit at Early Cretaceous.
WOS关键词	EAST-CENTRAL CHINA ; AU SKARN DEPOSIT ; RE-OS ; SOUTH CHINA ; BRITISH-COLUMBIA ; BROOKS RANGE ; SEDEX DEPOSITS ; GOLD DEPOSIT ; RIVER VALLEY ; ORE-DEPOSITS
WOS研究方向	Geology ; Mineralogy ; Mining & Mineral Processing
语种	英语
WOS记录号	WOS:000387625800054
资助机构	National Basic Research Program of China(2012CB416802) ; National Basic Research Program of China(2012CB416802) ; National Natural Science Foundation of China(41325007 ; National Natural Science Foundation of China(41325007 ; Nanjing Centre of China Geological Survey ; Nanjing Centre of China Geological Survey ; TOTAL endowment fund ; TOTAL endowment fund ; 91414301) ; 91414301) ; National Basic Research Program of China(2012CB416802) ; National Basic Research Program of China(2012CB416802) ; National Natural Science Foundation of China(41325007 ; National Natural Science Foundation of China(41325007 ; Nanjing Centre of China Geological Survey ; Nanjing Centre of China Geological Survey ; TOTAL endowment fund ; TOTAL endowment fund ; 91414301) ; 91414301)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/53274]
专题	地质与地球物理研究所_岩石圈演化国家重点实验室
作者单位	1.China Univ Geosci, Fac Earth Resources, Wuhan 430074, Peoples R China 2.Univ Durham, Dept Earth Sci, Durham DH1 3LE, England 3.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China 4.Bur Geol & Mineral Explorat Anhui Prov, Geol Team 321, Tongling 244033, Peoples R China 5.China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China
推荐引用方式 GB/T 7714	Li, Yang,Li, Jian-Wei,Li, Xian-Hua,et al. An Early Cretaceous carbonate replacement origin for the Xinqiao stratabound massive sulfide deposit, Middle-Lower Yangtze Metallogenic Belt, China[J]. ORE GEOLOGY REVIEWS,2017,80:985-1003.
APA	Li, Yang.,Li, Jian-Wei.,Li, Xian-Hua.,Selby, David.,Huang, Guang-Huan.,...&Zheng, Kai.(2017).An Early Cretaceous carbonate replacement origin for the Xinqiao stratabound massive sulfide deposit, Middle-Lower Yangtze Metallogenic Belt, China.ORE GEOLOGY REVIEWS,80,985-1003.
MLA	Li, Yang,et al."An Early Cretaceous carbonate replacement origin for the Xinqiao stratabound massive sulfide deposit, Middle-Lower Yangtze Metallogenic Belt, China".ORE GEOLOGY REVIEWS 80(2017):985-1003.