东天山卡拉塔格地区月牙湾铜镍硫化物矿床磁黄铁矿Re-Os同位素测定及其地质意义

吕晓强; 毛启贵; 郭娜欣; 李月臣; 孙燕

doi:10.3799/dqkx.2019.228

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3475-3486

Lü Xiaoqiang, Mao Qigui, Guo Naxin, Li Yuechen, Sun Yan, 2020. Re-Os Isotopic Dating of Pyrrhotite from Yueyawan Cu-Ni Sulfide Deposit in Kalatage Area of East Tianshan Mountain and Its Geological Significance. Earth Science, 45(9): 3475-3486. doi: 10.3799/dqkx.2019.228

Citation:

Lü Xiaoqiang, Mao Qigui, Guo Naxin, Li Yuechen, Sun Yan, 2020. Re-Os Isotopic Dating of Pyrrhotite from Yueyawan Cu-Ni Sulfide Deposit in Kalatage Area of East Tianshan Mountain and Its Geological Significance. Earth Science, 45(9): 3475-3486. doi: 10.3799/dqkx.2019.228

Citation:

Lü Xiaoqiang, Mao Qigui, Guo Naxin, Li Yuechen, Sun Yan, 2020. Re-Os Isotopic Dating of Pyrrhotite from Yueyawan Cu-Ni Sulfide Deposit in Kalatage Area of East Tianshan Mountain and Its Geological Significance. Earth Science, 45(9): 3475-3486. doi: 10.3799/dqkx.2019.228

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Re-Os Isotopic Dating of Pyrrhotite from Yueyawan Cu-Ni Sulfide Deposit in Kalatage Area of East Tianshan Mountain and Its Geological Significance

doi: 10.3799/dqkx.2019.228

Lü Xiaoqiang^{1
,
,},
Mao Qigui¹,
Guo Naxin^{2
,
,},
Li Yuechen¹,
Sun Yan¹

1.
Beijing Institute of Geology for Mineral Resources, Beijing 100012, China
2.
Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

Received Date: 2019-09-11
Publish Date: 2020-09-15

Abstract

Abstract

The Yueyawan Cu-Ni deposit is a newly discovered magmatic Cu-Ni sulfide deposit in Kalatage area of East Tianshan Mountain. In order to restrict the metallogenic age of the Yueyawan Cu-Ni deposit, LA-ICP-MS U-Pb and Re-Os isotopic dating had been conducted for zircons and pyrrhotite from the ore-forming olivine gabbro, respectively. The ²⁰⁶Pb/²³⁸U ages of zircons range from 255 Ma to 292 Ma, and yield an average weighted age of 274±2.4 Ma, which represents the diagenetic age of olivine gabbro. The isochron age of the Re-Os isotopic dating of pyrrhotite is 271.9±9.5 Ma, which represents the age of Cu-Ni mineralization. The initial ¹⁸⁷Os/¹⁸⁸Os ratio is 0.279 6±0.008 9, and γ_Os value is 117-126, indicating that crustal materials had been involved into the sulfide mineralization. The diagenesis and metallogenesis of mafic magma in Yueyawan occurred in Early Permian, contemporary with the typical Cu-Ni sulfide deposits in Huangshan-Tulaergen area of East Tianshan Mountain.
- mafic complex,
- Re-Os isotopic dating,
- Cu-Ni sulfide deposit,
- Yueyawan,
- East Tianshan Mountain,
- mineral deposits

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References(64)

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