宁夏卫宁北山金场子金矿床流体来源及矿床成因：来自流体包裹体和C-H-O同位素证据

海连富; 刘安璐; 陶瑞; 白金鹤; 宋扬

doi:10.3799/dqkx.2021.101

Volume 46 Issue 12

Dec. 2021

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Article Navigation > Earth Science > 2021 > 46(12): 4274-4290

Hai Lianfu, Liu Anlu, Tao Rui, Bai Jinhe, Song Yang, 2021. Source of Fluid and Genesis of Jinchangzi Gold Deposit in Weiningbeishan, Ningxia: Evidence from Fluid Inclusions and C-H-O Isotopes. Earth Science, 46(12): 4274-4290. doi: 10.3799/dqkx.2021.101

Citation:

Hai Lianfu, Liu Anlu, Tao Rui, Bai Jinhe, Song Yang, 2021. Source of Fluid and Genesis of Jinchangzi Gold Deposit in Weiningbeishan, Ningxia: Evidence from Fluid Inclusions and C-H-O Isotopes. Earth Science, 46(12): 4274-4290. doi: 10.3799/dqkx.2021.101

Citation:

Hai Lianfu, Liu Anlu, Tao Rui, Bai Jinhe, Song Yang, 2021. Source of Fluid and Genesis of Jinchangzi Gold Deposit in Weiningbeishan, Ningxia: Evidence from Fluid Inclusions and C-H-O Isotopes. Earth Science, 46(12): 4274-4290. doi: 10.3799/dqkx.2021.101

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Source of Fluid and Genesis of Jinchangzi Gold Deposit in Weiningbeishan, Ningxia: Evidence from Fluid Inclusions and C-H-O Isotopes

doi: 10.3799/dqkx.2021.101

Hai Lianfu^{1, 2, 3
,
,},
Liu Anlu^{4
,
,},
Tao Rui³,
Bai Jinhe³,
Song Yang³

1.
School of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
National Demonstration Center for Experimental Mineral Exploration Education, Wuhan 430074, China
3.
Mineral and Geological Survey Institute of Ningxia Hui Autonomous Region, Yinchuan 750021, China
4.
Yifu Museum of China University of Geosciences, Wuhan 430074, China

Received Date: 2021-04-03
Publish Date: 2021-12-15

Abstract

Abstract

The Weiningbeishan area is the most promising polymetallic ore target area in Ningxia, where numerous Au, Ag, Cu, Pb, Zn, Fe, Co, and other ore occurrences have been found. The Jinchangzi gold deposit is the largest gold deposit found in the area, and the ore bodies are mainly hosted in the intra-layer fault fractures, with an east-west distribution and near-uniform with the bedding. Magmatism is weak in this district, with several diorite porphyrite having been identified in exposures adjacent to the gold veins. In order to explore the nature, source and genesis of the ore-forming fluid of the Jinchangzi gold deposit, the fluid inclusions and C-H-O isotopes in the study area were studied. The ore-forming hydrothermal period of the deposit can be divided into 4 metallogenic stages, from early to late, they are sericite-pyrite-quartz stage (Ⅰ), pyrite-barite-quartz stage (Ⅱ), polymetallic sulfide-carbonate-quartz stage (Ⅲ) and pyrite-carbonatite stage (Ⅳ), of which stage Ⅲ is the main metallogenic stage. There are four types of fluid inclusions in the mineralization stage, which are aqueous solution inclusions, pure CO₂ inclusions, CO₂-H₂O inclusions and multiphase inclusions containing daughter crystals. The completely homogenous temperature of the ore-forming fluids is between 171-396℃, the salinity is between 1.30%-10.99% NaCl equiv, and the density is 0.24-0.78 g/cm³, which are CO₂-H₂O-NaCl systems with medium-low temperature, low salinity, low density, CO₂ rich, and a small amount of N₂. The δD value of hydrothermal quartz is -66.0‰ to -32.0‰, and the δ¹⁸O_V-SMOW value is (+19.7‰)-(+22.6‰), indicating that the ore-forming fluid is metamorphic and the magmatism is not obvious. The C isotope shows that the δ¹³C of calcite and siderite in the late stage (stage Ⅳ) is between -2.540‰ and -0.736‰, indicating that C in the ore-forming fluid has the characteristics of mixed sources. The fluids formed by the metamorphic dehydration of Ordovician-Carboniferous terrigenous clastic rocks and carbonate rocks may be the main source of gold ore-forming fluids. During the ore-forming process, the fluids had an obvious immiscibility phenomenon, which was an important factor causing gold precipitation. The genetic type of the deposit is an orogenic gold deposit.
- stable isotope,
- source of ore-forming fluid,
- genesis of ore deposit,
- fluid inclusions,
- Jinchangzi gold deposit,
- Weiningbeishan

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References(85)

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Source of Fluid and Genesis of Jinchangzi Gold Deposit in Weiningbeishan, Ningxia: Evidence from Fluid Inclusions and C-H-O Isotopes

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