Geological, Fluid Inclusion, H-O-S-Pb Isotope Constraints on the Genesis of the Erdaogou Gold Deposit, Liaoning Province

Fan Yang; Xuejiao Pang; Bin Li; Jingsheng Chen; Jilong Han; Miao Liu; Zhongzhu Yang; Yan Wang; Yi Shi

doi:10.1007/s12583-020-1068-5

Volume 32 Issue 1

Mar 2021

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Journal of Earth Science > 2021 > 32(1): 103-115.

Fan Yang, Xuejiao Pang, Bin Li, Jingsheng Chen, Jilong Han, Miao Liu, Zhongzhu Yang, Yan Wang, Yi Shi. Geological, Fluid Inclusion, H-O-S-Pb Isotope Constraints on the Genesis of the Erdaogou Gold Deposit, Liaoning Province. Journal of Earth Science, 2021, 32(1): 103-115. doi: 10.1007/s12583-020-1068-5

Citation:

Fan Yang, Xuejiao Pang, Bin Li, Jingsheng Chen, Jilong Han, Miao Liu, Zhongzhu Yang, Yan Wang, Yi Shi. Geological, Fluid Inclusion, H-O-S-Pb Isotope Constraints on the Genesis of the Erdaogou Gold Deposit, Liaoning Province. Journal of Earth Science, 2021, 32(1): 103-115. doi: 10.1007/s12583-020-1068-5

Citation:

Fan Yang, Xuejiao Pang, Bin Li, Jingsheng Chen, Jilong Han, Miao Liu, Zhongzhu Yang, Yan Wang, Yi Shi. Geological, Fluid Inclusion, H-O-S-Pb Isotope Constraints on the Genesis of the Erdaogou Gold Deposit, Liaoning Province. Journal of Earth Science, 2021, 32(1): 103-115. doi: 10.1007/s12583-020-1068-5

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Geological, Fluid Inclusion, H-O-S-Pb Isotope Constraints on the Genesis of the Erdaogou Gold Deposit, Liaoning Province

doi: 10.1007/s12583-020-1068-5

Fan Yang^{1, 2, 3
,},
Xuejiao Pang^{1
,
,
,},
Bin Li¹,
Jingsheng Chen¹,
Jilong Han⁴,
Miao Liu¹,
Zhongzhu Yang¹,
Yan Wang¹,
Yi Shi¹

1.
Shenyang Center of China Geological Survey, Shenyang 110034, China
2.
Scientific Research Department of Changchun University, Changchun 130022, China
3.
Natural Resources Comprehensive Survey Center of Mudanjiang, Mudanjiang 157000, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

More Information

Corresponding author: XuejiaoPang, 187117648@qq.com
Received Date: 15 Mar 2020
Accepted Date: 23 Jul 2020
Publish Date: 01 Feb 2021

Abstract

Abstract

The Erdaogou gold deposit is located in the conjuncture of North China Carton and Xingmeng orogenic belt. The ore-forming process of Erdaogou gold deposit is divided into three stages (Ⅰ to Ⅲ), which are quartz-pyrite stage (stage Ⅰ), quartz-polymetallic sulfide stage (stage Ⅱ) and quartz-calcite stage (stage Ⅲ). Two types of fluid inclusions is distinguished in the ore-forming stage, i.e., aqueous type (W-type) and aqueous-carbonic type (C-type) inclusions. From the stage Ⅰ to Ⅲ, the homogenization temperature of fluid inclusions are respectively 334-395, 214-364 and 172-272 ℃, with salinities of 7.72 wt.%-11.23 wt.% NaCl equiv., 0.20 wt.%-23.18 wt.% NaCl equiv., and 0.35 wt.% to 5.25 wt.% NaCl equiv. The ore-forming fluids of the Erdaogou deposit have the characteristics of medium-low temperatures, moderate salinities and low densities. And the fluids belong to the CO₂-H₂O-NaCl system. The values of δ³⁴S_V_-_CDT in sulphide samples at different stages (stages Ⅰ to Ⅲ) are between -2.2‰ to 2.3‰, indicating sulfur source from magma volatiles or subvolcanic rock leaching. The lead isotopes suggest that ore-forming metals may be derived from a mixture of lower crust and mantle materials. Oxygen and hydrogen isotope data at Erdaogou indicate that magmatic fluid and meteoric water may both be involved in the hydrothermal system. Based on the geological characteristics, fluid inclusion results, stable and radiogenic isotope results of Erdaogou gold deposit, we believe that the temperature decrease, fluid boiling are the key factors leading to the ore precipitation and the genetic type of Erdaogou gold deposit is low-sulfidation epithermal deposit.
- fluid inclusion,
- isotope systematic,
- ore genesis,
- Erdaogou gold deposit,
- Liaoning Province

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References(59)

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Geological, Fluid Inclusion, H-O-S-Pb Isotope Constraints on the Genesis of the Erdaogou Gold Deposit, Liaoning Province

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