The genesis of Qichun liemazui granite and its relationship with molybdenum mineralization

LIU Xin; ZHANG Sen; HONG Hanlie; JIN Shanhe; ZHONG Hui; WU Yue; JU Nan; SHI Lu

doi:10.12097/gbc.2022.03.021

2024 Vol. 43, No. 8

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LIU Xin, ZHANG Sen, HONG Hanlie, JIN Shanhe, ZHONG Hui, WU Yue, JU Nan, SHI Lu. 2024. The genesis of Qichun liemazui granite and its relationship with molybdenum mineralization. Geological Bulletin of China, 43(8): 1417-1429. doi: 10.12097/gbc.2022.03.021

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LIU Xin, ZHANG Sen, HONG Hanlie, JIN Shanhe, ZHONG Hui, WU Yue, JU Nan, SHI Lu. 2024. The genesis of Qichun liemazui granite and its relationship with molybdenum mineralization. Geological Bulletin of China, 43(8): 1417-1429. doi: 10.12097/gbc.2022.03.021

The genesis of Qichun liemazui granite and its relationship with molybdenum mineralization

1.
Shenyang Center of China Geological Survey (Northeast S & T Innovation Center), Shenyang 110034, Liaoning, China
2.
Cores and Samples Centre of Nature and Resources, Langfang 065201, Hebei, China
3.
China University of Geosciences(Wuhan), Wuhan 430074, Hubei, China

More Information

Corresponding author: ZHANG Sen, zhangsen556@163.com

Received Date: 01 March 2020

Revised Date: 29 May 2020

Publish Date: 15 August 2024

Abstract

Abstract

Qichun Liemazui molybdenum mine in Hubei Province is located on the southern slope of Dabie Mountain. Proven large molybdenum mines are rarely reported. There are few in−depth studies on this mining area, and there is a lack of accurate determination of the diagenetic and mineralization age, genesis and tectonic setting. In this paper, the Liemazui ore−forming granite was selected for petrographic, and petrochemical studies. The experimental results indicate that the ore−forming rocks are porphyry monzogranite or monzogranite−porphyry by petrographic analysis. The ore−forming scale of the mining area is small. The ore is disseminated or veined disseminated. The isochronous age of molybdenite in liemazui deposit is 119±8 Ma, the weighted mean age was 118.9±0.98 Ma. Therefore, the Liemazui molybdenum deposit is formed in the Early Cretaceous. Geochemical data show that it is a high−silicon, high−potassium, calc−alkaline series A−type granite. The total amount of rare earth elements is high, the light rare earth elements are enriched, and the heavy rare earth elements are relatively deficient. The rocks related to metallogenic formation in the Liemazui molybdenum mining area were formed in the extensional environment of the Dabie orogenic belt, and were related to the thinning of the lithosphere in the Late Yanshanian period.
- Liemazui granite /
- molybdenite /
- petrochemical /
- Re−Os isotopic dating /
- Hubei Provincce

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References

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