GYIG OpenIR  > 矿床地球化学国家重点实验室
Geochemical characteristics and metallogenesis of Carlin-type gold deposits in the Sandu-Danzhai metallogenic zone, Guizhou Province, China
YAN Baowen;  XIA Yong;  WANG Zepeng;  TAN Qingping;  WU Shourong;  FAN Erchuan
2012
Source PublicationChinese Journal of Geochemistry
Volume31Issue:3Pages:209-220
Abstract
Geochemical studies of the Paiting and Miaolong Carlin-type gold deposits in the Sandu-Danzhai metallogenic zone, Guizhou Province, have shown that the mineralized-altered rocks show LREE-enrichment patterns, generally displaying negative Eu anomalies (δEu=0.510.97) and unobvious negative Ce anomalies (δCe=0.860.99). Calcite and fluorite in relation with metallogenesis show MREE-enrichment patterns, generally displaying rather weak negative Eu anomalies (δEu=0.740.93) and weak negative Ce (δCe=0.700.98) anomalies.
The δ13CPDB values of carbon in calcite are -1.61‰ -5.82‰, the δ18OSMOW values of oxygen are 13.97‰19.24‰, and the δ34SCDT values of sulfur in stibnite are 17.72‰21.68‰. In regard to δD and δ18O, ore-forming fluids possess the characteristics of metamorphic water. The process of metallogenesis of the Carlin-type gold deposits is controlled by the Yanshanian tectonic activities. The Yanshanian movement promoted the migration and mobilization of metamorphic fluids in the extensively developed medium- to high-grade metamorphic rocks in this region, carrying primarily enriched gold and associated elements such as Hg, As, and Sb in the Sinian metamorphosed black shales and Lower Cambrian black shales. The ore-forming fluids found their way into a suitable metallogenic environment along the fault zone, followed by gold precipitation to form gold deposits.
KeywordCarlin-type Gold Deposit Geochemistry Paiting And Miaolong Gold Deposits Guizhou Province
Indexed ByEI
Language英语
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/42920512-1/10973
Collection矿床地球化学国家重点实验室
Affiliation1.State Key Lab. of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China
2.Postgraduate University of Chinese Academy of Sciences, Beijing 100039, China
3.No.1 General Party of Bureau of Non-ferrous Geological Exploration of Guizhou Province, Guiyang 551400, China
Recommended Citation
GB/T 7714
YAN Baowen;XIA Yong;WANG Zepeng;TAN Qingping;WU Shourong;FAN Erchuan. Geochemical characteristics and metallogenesis of Carlin-type gold deposits in the Sandu-Danzhai metallogenic zone, Guizhou Province, China[J]. Chinese Journal of Geochemistry,2012,31(3):209-220.
APA YAN Baowen;XIA Yong;WANG Zepeng;TAN Qingping;WU Shourong;FAN Erchuan.(2012).Geochemical characteristics and metallogenesis of Carlin-type gold deposits in the Sandu-Danzhai metallogenic zone, Guizhou Province, China.Chinese Journal of Geochemistry,31(3),209-220.
MLA YAN Baowen;XIA Yong;WANG Zepeng;TAN Qingping;WU Shourong;FAN Erchuan."Geochemical characteristics and metallogenesis of Carlin-type gold deposits in the Sandu-Danzhai metallogenic zone, Guizhou Province, China".Chinese Journal of Geochemistry 31.3(2012):209-220.
Files in This Item: Download All
File Name/Size DocType Version Access License
Geochemical characte(1757KB)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
[YAN Baowen;XIA Yong;WANG Zepeng;TAN Qingping;WU Shourong;FAN Erchuan]'s Articles
Baidu academic
Similar articles in Baidu academic
[YAN Baowen;XIA Yong;WANG Zepeng;TAN Qingping;WU Shourong;FAN Erchuan]'s Articles
Bing Scholar
Similar articles in Bing Scholar
[YAN Baowen;XIA Yong;WANG Zepeng;TAN Qingping;WU Shourong;FAN Erchuan]'s Articles
Terms of Use
No data!
Social Bookmark/Share
File name: Geochemical characteristics and metallogenesis of Carlin-type gold deposits in the Sandu-Danzhai metallogenic zone, Guizhou Province, China.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.