Ore-forming material sources and genesis of the Paishanlou gold deposit in the Liaoning Province, China: Constraints from the C-O-S-Pb isotope geochemistry of the T4 orebody

LIU Chunfa; LIU Yanbing; LIU Bizheng; XU Liwei

doi:10.19509/j.cnki.dzkq.tb20240306

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LIU Chunfa，LIU Yanbing，LIU Bizheng，et al. Ore-forming material sources and genesis of the Paishanlou gold deposit in the Liaoning Province, China: Constraints from the C-O-S-Pb isotope geochemistry of the T4 orebody[J]. Bulletin of Geological Science and Technology，2025，44（2）：1-15 doi: 10.19509/j.cnki.dzkq.tb20240306

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Ore-forming material sources and genesis of the Paishanlou gold deposit in the Liaoning Province, China: Constraints from the C-O-S-Pb isotope geochemistry of the T4 orebody

doi: 10.19509/j.cnki.dzkq.tb20240306

1.
China National Gold Group Hong Kong Co., Ltd., Beijing 100011, China
2.
School of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, China
3.
China Gold Group Resources Co., Ltd., Beijing 101300, China
4.
China Gold Group Geology Co., Ltd., Beijing 101300, China

More Information

Corresponding author: E-mail：lcfjlu704@163.com
Received Date: 06 Jun 2024
Accepted Date: 07 Aug 2024
Rev Recd Date: 23 Jul 2024

Available Online: 21 Mar 2025

Abstract

Abstract

Objective
The Paishanlou gold deposit is a large gold deposit on the northern margin of the North China Craton, containing more than 60 tons of gold resources. It is mainly hosted in Archean metamorphic rocks of the Jianping Group, structurally controlled by EW and NE ductile shear zones, and closely related to the Yanshanian granites. For many years, the genetic type of the Paishanlou gold deposit is still controversial.
Methods
In this study, we present new field geology and C-O-S-Pb isotope data for the T4 orebody in the Paishanlou deposit, in order to identify the ore-forming material sources and its genesis.
Results
The δ¹³C_V-PDB and the δ¹⁸O_V-SMOW values of hydrothermal carbonate minerals from ores range from −7.0‰ to −2.1‰ and 12.2‰ to 16.7‰ respectively. Compared with the Gaoyuzhuang Formation dolomitic marble, the δ¹⁸O_V-SMOW values are lower while the δ¹³C_V-PDB values are almost identical, indicating that the C isotope in the ore-forming fluid was derived from the dissolution of dolomitic marble in the Gaoyuzhuang Formation. The δ³⁴S values of pyrites from ores vary from 0.5‰ to 7.5‰ with two peak values (2.9‰ and 6.7‰), which correspond to δ³⁴S values of the metamorphic rocks of Jianping Group and the Yanshanian granitoids, indicating the sulfurs were mainly derived from a mixed source of the metamorphic rocks of Jianping Group and the Yanshanian magmatic sulfur. The Pb isotopic compositions of the pyrites from ores vary from 16.585 to 18.432, 15.299 to 15.698 and 37.159 to 38.982 for ²⁰⁶Pb/²⁰⁴Pb, ²⁰⁷Pb/²⁰⁴Pb and ²⁰⁸Pb/²⁰⁴Pb ratios respectively, which plot between the mantle and lower crust fields in the ²⁰⁷Pb/ ²⁰⁴ Pb versus ²⁰⁶Pb/ ²⁰⁴ Pb discrimination diagrams, indicating a mixed source of crust and mantle. Thus, we suggest the ore-forming metals were derived from a mixed source of metamorphic rock of Jianping Group and the Yanshanian granitoids.
Conclusion
Combined with the regional tectono-magmatic evolution history during the Mesozoic, we propose that the NE ductile shearing in the Paishanlou district resulted in dynamic metamorphism of Precambrian country rocks to form ore-bearing metamorphic fluid under the background of the regional extensional tectonism and lithosphere thinning during the late Cretaceous. During the migration of the ore-forming fluid along the ductile shear zone, the meteoric water, magmatic hydrothermal fluid and ore-forming materials from the country rocks were involved in it, resulting in the characteristics of crust-mantle mixing. Finally, in the favorable environment such as tectonic intersection or dolomitic marble interface, the ore-forming fluid reacted with the country rock, leading to the rapid precipitation of ore-forming materials. The Paishanlou gold deposit belongs to orogenic gold deposit.
- Paishanlou gold deposit,
- C-O-S-Pb isotope,
- ore-forming material source,
- orogenic gold deposit,
- northeastern margin of North China Craton,
- geochemistry

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References(62)

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Ore-forming material sources and genesis of the Paishanlou gold deposit in the Liaoning Province, China: Constraints from the C-O-S-Pb isotope geochemistry of the T4 orebody

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Ore-forming material sources and genesis of the Paishanlou gold deposit in the Liaoning Province, China: Constraints from the C-O-S-Pb isotope geochemistry of the T4 orebody

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