赣南樟东坑钨矿两类矿化中辉钼矿的Re-Os同位素定年及其地质意义

李光来; 华仁民; 韦星林; 屈文俊; 黄小娥; 胡东泉; 周龙全

doi:10.3799/dqkx.2014.016

Volume 39 Issue 2

Feb. 2014

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Article Navigation > Earth Science > 2014 > 39(2): 165-173

Li Guanglai, Hua Renmin, Wei Xinglin, Qu Wenjun, Huang Xiaoe, Hu Dongquan, Zhou Longquan, 2014. Re-Os Isotopic Ages of Two Types of Molybdenite from Zhangdongkeng Tungsten Deposit in Southern Jiangxi Province and Their Geologic Implications. Earth Science, 39(2): 165-173. doi: 10.3799/dqkx.2014.016

Citation:

Li Guanglai, Hua Renmin, Wei Xinglin, Qu Wenjun, Huang Xiaoe, Hu Dongquan, Zhou Longquan, 2014. Re-Os Isotopic Ages of Two Types of Molybdenite from Zhangdongkeng Tungsten Deposit in Southern Jiangxi Province and Their Geologic Implications. Earth Science, 39(2): 165-173. doi: 10.3799/dqkx.2014.016

Citation:

Li Guanglai, Hua Renmin, Wei Xinglin, Qu Wenjun, Huang Xiaoe, Hu Dongquan, Zhou Longquan, 2014. Re-Os Isotopic Ages of Two Types of Molybdenite from Zhangdongkeng Tungsten Deposit in Southern Jiangxi Province and Their Geologic Implications. Earth Science, 39(2): 165-173. doi: 10.3799/dqkx.2014.016

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Re-Os Isotopic Ages of Two Types of Molybdenite from Zhangdongkeng Tungsten Deposit in Southern Jiangxi Province and Their Geologic Implications

doi: 10.3799/dqkx.2014.016

1.
State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China Institute of Technology, Nanchang 330013, China
2.
State Key Laboratory of Mineral Deposits Research, Nanjing University, Nanjing 210093, China
3.
Jiangxi Nonferrous Metal Geological Exploration Bureau, Nanchang 330025, China
4.
National Research Center for Geoanalysis, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2013-04-30
Publish Date: 2014-02-01

Abstract

Abstract

Zhangdongkeng tungsten deposit has a special mineralization model, which is a quartz vein type mineralization in the upper portion while an altered granite type mineralization in the lower part. It also shows that tungsten was enriched in the upper part while molybdenum enriched in the lower. Molybdenites in fine-grained granite and quartz vein were separately used for Re-Os dating to test the temporal relation of the two types of mineralization. The isochron age of three molybdenite samples in fine-grained granite is 155.4±2.1 Ma (MSWD=1.12), with model ages of them between 154.9±2.6 Ma and 156.5±2.6 Ma, and the weighted average age 155.5±1.4 Ma (MSWD=0.44). Five molybdenite samples in quartz vein yield a Re-Os isochron age of 154.6±1.7 Ma (MSWD=0.030), with model ages 154.2±2.3 Ma to 154.7±2.7 Ma, and the weighted mean age is 154.29±0.98 Ma (MSWD=0.045). The results show that the ages of altered granite type mineralization and quartz vein type mineralization are basically almost same, which well indicates that molybdenites in both mineralization types are products of the same magmatic-hydrothermal event.
- quartz vein type mineralization,
- altered granite type mineralization,
- molybdenite,
- geochronology,
- Zhangdongkeng

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References(76)

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Re-Os Isotopic Ages of Two Types of Molybdenite from Zhangdongkeng Tungsten Deposit in Southern Jiangxi Province and Their Geologic Implications

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