GYIG OpenIR  > 矿床地球化学国家重点实验室
Origin of the Wangpingxigou Pb-Zn deposit in East Qinling orogenic belt,China: Distal response to the giant Donggou porphyry Mo system?
Chang Jin;  Wei Terry Chen;  Xin-Yu Gao;  Xiao-Chun Li;   Zhi-Wei Bao;  Tai-Ping Zhao
2019
Source PublicationOre Geology Reviews
Volume109Pages:101–116
Abstract

The southern margin of the North China Craton (NCC) hosts many world-class porphyry Mo and vein-type PbZn ± Ag deposits, forming an important polymetallic metallogenic belt in China, even over the world. Although the Mo and Pb-Zn ± Ag mineralization are temporarily and spatially associated with each other, their possible genetic links are still unclear. To delineate the relationships between the two types of ore mineralization, we carried out in-situ geochemical and S-Pb isotopic analyses on sulfides from the two spatially associated deposits, i.e., the Wangpingxigou Pb-Zn and Donggou porphyry Mo deposits in the ore district. Based on field and microscopic observations on the crosscutting relationships of various veins and paragenetic relationships of various hydrothermal minerals, three (I–III) and four (I–IV) stages of hydrothermal veins have been identified in the Wangpingxigou and Donggou deposits, respectively. Pyrite grains from stage II of the Wangpingxigou deposit have high Co/Ni ratios (mostly > 1) and Au and As contents similar to those of typical epithermal systems. Moreover, sulfides from this deposit have in-situ 206Pb/204Pb (17.345–17.417), 207Pb/204Pb (15.454–15.514), and 208Pb/204Pb (38.138–38.364) ratios similar to those of sulfides from the Donggou deposit, indicating that the two deposits were relevant to a common source. The concentrations of many elements (i.e. Pb, Ag, Sn, Zn, Sb, Mn, Au and As) in pyrite decrease gradually from the stage II of the Wangpingxigou deposit to the stage II of the Donggou deposit, consistent with metal zonation typically observed in porphyry related metallogenic systems. Further considering similar ages of the two deposits, we propose that the Wangpingxigou Pb-Zn deposit is likely distal to the Donggou porphyry Mo system. The range of δ34S values of pyrites (7.63–8.76‰) from the stage II in the Donggou deposit is similar to those of the ancient strata (Xiong’er Group) (7.31–8.17‰) in the ore district, indicating that the sulfur in ore-forming fluids may be mainly derived from the ancient strata. However, the δ34S values (9.20–9.70‰) of Stage III sulfides in the Donggou deposit are higher than those of stage II sulfides in the Donggou deposit and stage II sulfides in the Wangpingxigou deposit (7.34–9.29‰). The different sulfur isotopic compositions may be related to varied physicochemical conditions of the ore-forming fluids. Confirmation of a Mo-Pb-Zn metallogenic system in the region provides important clues on further prospecting of Mo and Pb-Zn resources in the southern margin of the North China Craton.

KeywordSulfides in-situ s Isotopes in-situ Pb Isotopes in-situ Trace Elements donggou Porphyry Mo Deposit a Metallogenic System
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/10548
Collection矿床地球化学国家重点实验室
Affiliation1.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China
2.Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
3.Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, China
Recommended Citation
GB/T 7714
Chang Jin;Wei Terry Chen;Xin-Yu Gao;Xiao-Chun Li; Zhi-Wei Bao;Tai-Ping Zhao. Origin of the Wangpingxigou Pb-Zn deposit in East Qinling orogenic belt,China: Distal response to the giant Donggou porphyry Mo system?[J]. Ore Geology Reviews,2019,109:101–116.
APA Chang Jin;Wei Terry Chen;Xin-Yu Gao;Xiao-Chun Li; Zhi-Wei Bao;Tai-Ping Zhao.(2019).Origin of the Wangpingxigou Pb-Zn deposit in East Qinling orogenic belt,China: Distal response to the giant Donggou porphyry Mo system?.Ore Geology Reviews,109,101–116.
MLA Chang Jin;Wei Terry Chen;Xin-Yu Gao;Xiao-Chun Li; Zhi-Wei Bao;Tai-Ping Zhao."Origin of the Wangpingxigou Pb-Zn deposit in East Qinling orogenic belt,China: Distal response to the giant Donggou porphyry Mo system?".Ore Geology Reviews 109(2019):101–116.
Files in This Item: Download All
File Name/Size DocType Version Access License
Origin of the Wangpi(14350KB)期刊论文作者接受稿开放获取CC BY-NC-SAView Download
Related Services
Recommend this item
Bookmark
Usage statistics
Export to Endnote
Google Scholar
Similar articles in Google Scholar
[Chang Jin;Wei Terry Chen;Xin-Yu Gao;Xiao-Chun Li; Zhi-Wei Bao;Tai-Ping Zhao]'s Articles
Baidu academic
Similar articles in Baidu academic
[Chang Jin;Wei Terry Chen;Xin-Yu Gao;Xiao-Chun Li; Zhi-Wei Bao;Tai-Ping Zhao]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[Chang Jin;Wei Terry Chen;Xin-Yu Gao;Xiao-Chun Li; Zhi-Wei Bao;Tai-Ping Zhao]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: Origin of the Wangpingxigou Pb-Zn deposit in East Qinling orogenic belt, China_ Distal response to the giant Donggou porphyry Mo system_.pdf
Format: Adobe PDF
This file does not support browsing at this time
All comments (0)
No comment.
 

Items in the repository are protected by copyright, with all rights reserved, unless otherwise indicated.