胶东水旺庄金矿床成矿机制：来自S-H-O同位素和流体包裹体的制约

李杰; 张丽鹏; 宋明春; 梁金龙; 李世勇; 宋英昕; 鲍中义; 丁正江

doi:10.3799/dqkx.2020.358

Volume 46 Issue 5

May 2021

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Article Navigation > Earth Science > 2021 > 46(5): 1569-1584

Li Jie, Zhang Lipeng, Song Mingchun, Liang Jinlong, Li Shiyong, Song Yingxin, Bao Zhongyi, Ding Zhengjiang, 2021. Formation Mechanism of Shuiwangzhuang Gold Deposit in Jiaodong Peninsula: Constraints from S-H-O Isotopes and Fluid Inclusions. Earth Science, 46(5): 1569-1584. doi: 10.3799/dqkx.2020.358

Citation:

Li Jie, Zhang Lipeng, Song Mingchun, Liang Jinlong, Li Shiyong, Song Yingxin, Bao Zhongyi, Ding Zhengjiang, 2021. Formation Mechanism of Shuiwangzhuang Gold Deposit in Jiaodong Peninsula: Constraints from S-H-O Isotopes and Fluid Inclusions. Earth Science, 46(5): 1569-1584. doi: 10.3799/dqkx.2020.358

Citation:

Li Jie, Zhang Lipeng, Song Mingchun, Liang Jinlong, Li Shiyong, Song Yingxin, Bao Zhongyi, Ding Zhengjiang, 2021. Formation Mechanism of Shuiwangzhuang Gold Deposit in Jiaodong Peninsula: Constraints from S-H-O Isotopes and Fluid Inclusions. Earth Science, 46(5): 1569-1584. doi: 10.3799/dqkx.2020.358

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Formation Mechanism of Shuiwangzhuang Gold Deposit in Jiaodong Peninsula: Constraints from S-H-O Isotopes and Fluid Inclusions

doi: 10.3799/dqkx.2020.358

1.
Hebei Key Laboratory of Strategic Critical Mineral Resources, Hebei GEO University, Shijiazhuang 050031, China
2.
College of Earth Sciences, Hebei GEO University, Shijiazhuang 050031, China
3.
Center of Deep Sea Research, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
4.
Shandong Provincial No. 6 Exploration Institute of Geology and Mineral Resources, Weihai 264209, China
5.
College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China
6.
Shandong Institute of Geophysical and Geochemical Exploration, Jinan 250013, China
7.
Institute of Geological Sciences of Shandong Province, Jinan 250013, China
8.
Shandong Bureau of Geology and Mineral Resources Exploration and Development, Jinan 250013, China

Received Date: 2020-08-17
Publish Date: 2021-05-15

Abstract

Abstract

In order to discuss the genesis of the Shuiwangzhuang gold deposit in Jiaodong Peninsula, S-H-O isotopic compositions of gold-bearing pyrite and quartz were carried out, and the fluid inclusions in quartz during ore-forming period were analyzed in this study. The results show that the δ³⁴S of pyrite ranges from 7.0‰ to 8.5‰, with an average value of 7.7‰. The sulfur may be mainly from mantle sulfur and mixed with a small amount of crust sulfur. The δD of fluid in quartz ranges from -91.7 ‰ to -82.6 ‰, and δ¹⁸O_H2O ranges from 2.6 ‰ to 5.6 ‰, indicating that the ore-forming fluid is mainly magmatic water, and meteoric water was mixed in at the later stage of mineralization. Three types of fluid inclusions in quartz are recognized during the main metallogenic period, including gas-liquid two-phase fluid inclusions, CO₂-bearing fluid inclusions, and liquid rich fluid inclusions with daughter mineral. The salinity of fluid is between 1.2% and 13.8% (NaCl_eq), and the homogenization temperature is mainly concentrated between 290 and 350 ℃, indicating the main ore-forming fluid is H₂O-CO₂-NaCl±CH₄ system with medium-high temperature and low salinity. The immiscibility (phase separation) or boiling of fluid leads to the precipitation and enrichment of gold. In the Mesozoic, under the influence of the subduction and rollback of the paleo-Pacific plate, large-scale magmatic activities and strong crustal uplift occurred in Jiaodong Peninsula, and the resulting thermal uplift-extensional structure provided favorable conditions for the concentrated mineralization of large-scale gold deposits. In the main detachment fault, the high degree of rock fragmentation is conducive to atmospheric water infiltration, circulation and mixing with deep fluid to form altered rock type gold deposit in fracture zone. In the footwall of main detachment fault, the fracture scale is small and the connectivity with the surface is poor, which is not conducive to the infiltration of meteoric water. The ore-forming fluid is mainly deep-source fluid, forming quartz vein type gold deposit.
- Shuiwangzhuang gold deposit,
- sulfur isotope,
- hydrogen and oxygen isotopes,
- fluid inclusion,
- Jiaodong Peninsula,
- mineral deposit

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Formation Mechanism of Shuiwangzhuang Gold Deposit in Jiaodong Peninsula: Constraints from S-H-O Isotopes and Fluid Inclusions

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