吉林荒沟山金矿床成矿流体特征

周向斌; 李剑锋; 王可勇; 梁一鸿; 张淼; 韦烈民; 王志高

doi:10.3799/dqkx.2016.009

Volume 41 Issue 1

Jan. 2016

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Article Navigation > Earth Science > 2016 > 41(1): 121-130

Zhou Xiangbin, Li Jianfeng, Wang Keyong, Liang Yihong, Zhang Miao, Wei Liemin, Wang Zhigao, 2016. Geochemical Characteristics of Ore-Forming Fluid inHuanggoushan Gold Deposit, Jilin Province. Earth Science, 41(1): 121-130. doi: 10.3799/dqkx.2016.009

Citation:

Zhou Xiangbin, Li Jianfeng, Wang Keyong, Liang Yihong, Zhang Miao, Wei Liemin, Wang Zhigao, 2016. Geochemical Characteristics of Ore-Forming Fluid inHuanggoushan Gold Deposit, Jilin Province. Earth Science, 41(1): 121-130. doi: 10.3799/dqkx.2016.009

Citation:

Zhou Xiangbin, Li Jianfeng, Wang Keyong, Liang Yihong, Zhang Miao, Wei Liemin, Wang Zhigao, 2016. Geochemical Characteristics of Ore-Forming Fluid inHuanggoushan Gold Deposit, Jilin Province. Earth Science, 41(1): 121-130. doi: 10.3799/dqkx.2016.009

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Geochemical Characteristics of Ore-Forming Fluid inHuanggoushan Gold Deposit, Jilin Province

doi: 10.3799/dqkx.2016.009

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Heilongjiang Institute of Geological Science, Haerbin 150090, China
3.
College of Urban and Environmental Sciences, Liaoning Normal University, Dalian 116029, China
4.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2015-09-01
Publish Date: 2016-01-15

Abstract

Abstract

Occurred in Zhenzhumen Formation of Laoling Group of Proterozoic Era and controlled by ductile shear belt, the Huanggoushan gold deposit is one of the most representative deposits in Laoling gold-polymetallic metallogenic belt in southern Jilin Province. Based on the geological characteristics, mineral assemblage and the crosscutting relationship between different kinds of veins, the hydrothermal mineralization processes can be divided into two main stages, namely, stageⅠpyrite arsenopyrite quartz and stageⅡ later stibnite-milky quartz. Systematic study on petrography and microthermometry of fluid inclusions shows that quartz of Stage Ⅰcontains three types of primary fluid inclusions, which are CO₂ bearing three phases, carbonic and aqueous two phases inclusions respectively, and the ore forming fluid is of medium to low temperature and low salinity NaCl-H₂O-CO₂ kind of solutions and immiscibility happened in the ore forming process, which led to the enrichment of gold etc; in quartz of Stage Ⅱ, there are aqueous two phases fluids only and ore forming fluid is of homogeneous NaCl-H₂O kind of solutions. Isotopic studies of carbon, hydrogen and oxygen show that the ore forming fluids of mineralization Stage Ⅰ mainly derived from magmatic solutions, whereas fluids of mineralization stage Ⅱ mainly came from meteoric water in addition to the relicts of stage Ⅰ ore forming solutions. The values of δD and δ¹³C_V-PDB reveal that the ore forming fluids of both mineralization Stage Ⅰ and Ⅱ all experienced strong rock water reaction. The genesis of the gold deposit is medium temperature magmatic hydrothermal deposit.
- Huanggoushan gold deposit,
- ore-forming fluid,
- geochemical characteristics,
- ore genesis,
- southern Jilin Province.

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References(44)

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Geochemical Characteristics of Ore-Forming Fluid inHuanggoushan Gold Deposit, Jilin Province

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