A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton

doi:10.1016/j.oregeorev.2023.105492

GIG OpenIR

	Wang, Yongbin 1,2,3,4; Cai, Jiaqi 1,2; Liu, Li 5; Zhou, Jiaxi 2,3; Feng, Peiling 1,2; Guo, Yunkang 1,2; Lin, Song 1,2; Guo, Yunpeng 6
	A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton
刊名	ORE GEOLOGY REVIEWS
ISSN号	0169-1368
	2023-07-01
卷号	158 页码:15
DOI	10.1016/j.oregeorev.2023.105492
语种	英语
WOS研究方向	Geology ; Mineralogy ; Mining & Mineral Processing
摘要	Recent Pb-Zn-Ag exploration in the northern margin of North China Craton has made significant new discov-eries. Here we report one Pb-Zn-Ag deposit in the Shaolanghe orefield with typical signatures of intermediate-sulfidation epithermal deposits. Zhangjiagou Pb-Zn-Ag mineralization occurs within the Early Permian quartz diorite and Late Permian andesite. Three mineralization stages were identified: white quartz--rhodochrosite-sulfide Pb-Zn-mineralization stage (I), smoky quartz-sulfide Pb-Zn-Ag-mineralization stage (II), and calcite-quartz non-mineralization stage (III). Four sphalerite samples yield the Rb-Sr age of 265.3 Ma, indicating that Pb-Zn-Ag mineralization was associated with the Late Permian andesite. The liquid-rich fluid inclusions of Stage I show low-medium temperatures of 190-270 degrees C and low salinities (1-3 wt%), and those of Stage III are slightly lower (190-250 degrees C, 0.5-2 wt%), suggesting a low-salinity, low-temperature H2O-NaCl fluid system for the Zhangjiagou deposit. The H-O-C isotopic signatures indicate a mixed fluid of magmatic water with meteoric water. S and Pb isotopes suggest magmatic source for Zhangjiagou Pb-Zn-Ag mineralization, most likely shallow hydrous intermediate magma. Collectively, these geological, geochronological, and geochemical features indicate that Zhangjiagou is an intermediate-sulfidation epithermal Pb-Zn-Ag deposit.
关键词	Zhajiagou Pb Zn-Ag deposit Intermediate-sulfidation epithermal deposit Rb-Sr dating H-O-C-S-Pb isotope
WOS记录号	WOS:001008565400001
收录类别	SCI
引用统计	被引频次：1[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.gig.ac.cn/handle/344008/74354
专题	中国科学院广州地球化学研究所
通讯作者	Guo, Yunpeng
作者单位	1.Yunnan Univ, Yunnan Key Lab Earth Syst Sci, Kunming 650500, Peoples R China 2.Yunnan Univ, Key Lab Crit Minerals Metallogeny Univ Yunnan Prov, Kunming 650500, Peoples R China 3.MNR, Key Lab Sanjiang Metallogeny & Resources Explorat, Kunming 650051, Peoples R China 4.Yunnan Key Lab Sanjiang Metallogeny & Resources Ex, Kunming 650051, Peoples R China 5.Chinese Acad Sci, Guangzhou Inst Geochem, Guangzhou 510640, Peoples R China 6.Capital Normal Univ, Beijing 100048, Peoples R China
推荐引用方式 GB/T 7714	Wang, Yongbin,Cai, Jiaqi,Liu, Li,et al. A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton[J]. ORE GEOLOGY REVIEWS,2023,158:15.
APA	Wang, Yongbin.,Cai, Jiaqi.,Liu, Li.,Zhou, Jiaxi.,Feng, Peiling.,...&Guo, Yunpeng.(2023).A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton.ORE GEOLOGY REVIEWS,158,15.
MLA	Wang, Yongbin,et al."A Permian intermediate-sulfidation epithermal Pb-Zn-Ag deposit in the northern margin of North China Craton".ORE GEOLOGY REVIEWS 158(2023):15.