Zircon U-Pb ages, geochemical characteristics and their constraints on metallogenic mechanism of ore-bearing porphyry in Qingshuihe Donggou molybdenum deposit, East Kunlun

ZHANG Yong; MA Zhongyuan; LI Xiaowei; KUI Mingjuan; LIU Zhigang; MO Shengjuan

doi:10.12097/gbc.2024.05.047

2025 Vol. 44, No. 4

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ZHANG Yong, MA Zhongyuan, LI Xiaowei, KUI Mingjuan, LIU Zhigang, MO Shengjuan. 2025. Zircon U-Pb ages, geochemical characteristics and their constraints on metallogenic mechanism of ore-bearing porphyry in Qingshuihe Donggou molybdenum deposit, East Kunlun. Geological Bulletin of China, 44(4): 679-704. doi: 10.12097/gbc.2024.05.047

Citation:

ZHANG Yong, MA Zhongyuan, LI Xiaowei, KUI Mingjuan, LIU Zhigang, MO Shengjuan. 2025. Zircon U-Pb ages, geochemical characteristics and their constraints on metallogenic mechanism of ore-bearing porphyry in Qingshuihe Donggou molybdenum deposit, East Kunlun. Geological Bulletin of China, 44(4): 679-704. doi: 10.12097/gbc.2024.05.047

Zircon U-Pb ages, geochemical characteristics and their constraints on metallogenic mechanism of ore-bearing porphyry in Qingshuihe Donggou molybdenum deposit, East Kunlun

1.
The Third Geological Exploration Institute of Qinghai Province, Xining 810029, Qinghai, China
2.
School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China

More Information

Corresponding author: MA Zhongyuan, 44572386@qq.com

Received Date: 27 May 2024

Revised Date: 06 September 2024

Publish Date: 15 April 2025

Abstract

Abstract

Objective
The Qingshuihe Donggou porphyry molybdenum deposit is one of the representative porphyry deposits in the East Kunlun metallogenic belt.
Methods
Therefore, a detailed study of the age, genesis and tectonic environment of the porphyry intrusions in the Qingshuihe Donggou deposit is needed to improve the understanding of the metallogenic regularity of this area. In this paper, zircon U−Pb dating, petrogeochemistry and zircon Hf isotope of the porphyries from the Qingshuihe Donggou deposit, which are closely related to the Mo mineralization, have been studied.
Results
The zircon U−Pb age of granodiorite porphyry is 226.9 ± 1.3 Ma (MSWD = 1.03, n = 18), and the zircon U−Pb age of diorite porphyry is 224.3 ± 1.2 Ma (MSWD = 0.47, n = 15), These results indicate that this deposit formed at 226.9~224.3 Ma. Granodiorite porphyry, diorite porphyry and granite porphyry are rich in Si, Na, K and Al, poor in Ti and Mg, and show a right−leaning partition pattern characterized by the light rare earth element enrichment. The former two granites have no obvious Eu depletion (δEu: 0.79~0.98), whereas granite porphyry displays noticeable Eu depletion (δEu: 0.22~0.24). All of them are enriched in large ion lithophile elements (e.g., Rb, K, Ba), and depleted in high field strength elements (e.g., Ta, Nb, Ti, P), belonging to the metalluminous to weak peraluminous high K calc−alkaline granites. The ¹⁷⁶Hf/¹⁷⁷Hf ratio of zircon from these porphyry rocks ranges from 0.282510 to 0.282652, the ε_Hf(t) value ranges from −4.5 to 0.2, and the two−stage model age ranges from 1541 Ma to 1240 Ma.
Conclusions
Based on the characteristics of regional tectonic evolution, it is deduced that these porphyries formed by partial melting of the Middle Proterozoic Jinshuikou Group under the Late Triassic post−collisional extension environment, and experienced magma mixing by mantle−derived materials.
- porphyry molybdenum deposit /
- zircon U−Pb age /
- geochemistry /
- granodiorite porphyry /
- Qingshuihe Donggou /
- East Kunlun

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References

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