冈底斯中段岗讲斑岩铜钼矿床锆石U-Pb和辉钼矿Re-Os年代学及其地质意义

杨震; 姜华; 杨明国; 梅红波; 胡光道; 张黎黎; 张裴培

doi:10.3799/dqkx.2017.026

Volume 42 Issue 3

Mar. 2017

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Article Navigation > Earth Science > 2017 > 42(3): 339-356

Yang Zhen, Jiang Hua, Yang Mingguo, Mei Hongbo, Hu Guangdao, Zhang Lili, Zhang Peipei, 2017. Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance. Earth Science, 42(3): 339-356. doi: 10.3799/dqkx.2017.026

Citation:

Yang Zhen, Jiang Hua, Yang Mingguo, Mei Hongbo, Hu Guangdao, Zhang Lili, Zhang Peipei, 2017. Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance. Earth Science, 42(3): 339-356. doi: 10.3799/dqkx.2017.026

Citation:

Yang Zhen, Jiang Hua, Yang Mingguo, Mei Hongbo, Hu Guangdao, Zhang Lili, Zhang Peipei, 2017. Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance. Earth Science, 42(3): 339-356. doi: 10.3799/dqkx.2017.026

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Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance

doi: 10.3799/dqkx.2017.026

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Faculty of Land Resources Engineering, Kunming University of Science and Technology, Kunming 650093, China
3.
Yunnan Copper Industry (Group) Co., Ltd, Kunming 650051, China
4.
No. 326 Geological Team, Bureau of Geology and Mineral Exploration of Anhui Province, Anqing 246003, China
5.
Lhasa Tianli Mining Co., Ltd, Lhasa 850015, China

Received Date: 2016-10-01
Publish Date: 2017-03-15

Abstract

Abstract

The Gangjiang Copper-Molybdenum deposit is a typical porphyry deposit, which locates in the Central Gangdese metallogenic belt. In order to determine the ages of magmatism and mineralization, and disentangle the complicated magmatic evolution and the relationship between magmatic process and copper-molybdenum mineralization, the author carried out a study of LA-ICP-MS zircon U-Pb ages of the monzogranite porphyry, granodiorite porphyry, and tonalite porphyrite in Gangjiang mining area. It is shown that the zircon U-Pb weighted isochron ages are 16.6±0.3 Ma (MSWD=0.94, n=10), 16.1±0.2 Ma (MSWD=1.07, n=12), 14.4±0.4 Ma (MSWD=1.12, n=7). Meanwhile, twelve molybdenite samples separated from quartz sulfides in Gangjiang copper orebodies were used for Re-Os dating, and the model ages obtained range from 13.24±0.20 Ma to 13.55±0.22 Ma, with weighted average 13.4±0.1 Ma (MSWD=0.65) and isochron age 13.6±1.6 Ma (MSWD=1.2). On the basis of geological studies, and conbined with the results mentioned above and previous research data, it is proposed that the rock mass intrusion sequence is monzogranite porphyry→granodiorite porphyry→tonalite porphyrite→rhyolite porphyry. The porphyry occurred ranges from 16.6 Ma to 14.4 Ma, and the mineralization age of Gangjiang deposit is about 13.4 Ma, and petrogenetic and metallogenic is a continuous process of magmatic evolution. The Re content of the molybdenite is 155.4-171.1 μg/g, with an average of 162.9 μg/g, suggesting that the metallogenic material originated from a source with mantle components. Gangjiang porphyry copper-molybdenum deposit was formed in post-collisional extension setting of India-Asia continental collision orogenic belt during the Miocene.
- geochemistry,
- zircon U-Pb dating,
- molybdenite Re-Os dating,
- porphyry Cu-Mo deposit,
- Gangdese

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References(134)

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Zircon U-Pb and Molybdenite Re-Os Dating of the Gangjiang Porphyry Cu-Mo Deposit in Central Gangdese and Its Geological Significance

doi: 10.3799/dqkx.2017.026

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