青海玉树尕龙格玛VMS型矿床流体包裹体及H-O-S-Pb同位素特征

王键; 孙丰月; 禹禄; 姜和芳; 王飞; 宁传奇

doi:10.3799/dqkx.2017.074

Volume 42 Issue 6

Jun. 2017

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Article Navigation > Earth Science > 2017 > 42(6): 941-956

Wang Jian, Sun Fengyue, Yu Lu, Jiang Hefang, Wang Fei, Ning Chuanqi, 2017. Fluid Inclusions and H-O-S-Pb Isotope Systematics of the Galonggema Cu Deposit in Yushu, Qinghai Province, China. Earth Science, 42(6): 941-956. doi: 10.3799/dqkx.2017.074

Citation:

Wang Jian, Sun Fengyue, Yu Lu, Jiang Hefang, Wang Fei, Ning Chuanqi, 2017. Fluid Inclusions and H-O-S-Pb Isotope Systematics of the Galonggema Cu Deposit in Yushu, Qinghai Province, China. Earth Science, 42(6): 941-956. doi: 10.3799/dqkx.2017.074

Citation:

Wang Jian, Sun Fengyue, Yu Lu, Jiang Hefang, Wang Fei, Ning Chuanqi, 2017. Fluid Inclusions and H-O-S-Pb Isotope Systematics of the Galonggema Cu Deposit in Yushu, Qinghai Province, China. Earth Science, 42(6): 941-956. doi: 10.3799/dqkx.2017.074

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Fluid Inclusions and H-O-S-Pb Isotope Systematics of the Galonggema Cu Deposit in Yushu, Qinghai Province, China

doi: 10.3799/dqkx.2017.074

College of Earth Sciences, Jilin University, Changchun 130061, China

Received Date: 2016-12-10
Publish Date: 2017-06-15

Abstract

Abstract

In order to determine the metallogenic physicochemical condition, ore-forming materials, ore-forming fluid and metallogenic mechanism of Galonggema VMS (volcanogenic massive sulfide) deposit in the northern Sanjiang metallogenic belt, China, orebody features, fluid inclusion microthermometry, laser Raman spectroscopy, and S, Pb, H, O isotopes are studied in this paper. It is found that deposit is hosted in the Late Triassic Batang Group dacite-volcanic tuff and consists of two parts, namely, lower ore belt of vein-stockwork mineralization system belonging to hydrothermal fluid supply channel, and upper ore belt of exhalative-chemical deposit system of submarine basin brine pond. Fluid inclusions (FIs) in vein-stockwork mineralization are both aqueous and gas-rich, homogenization temperature from 175.6 to 263.3 ℃, and salinities of 1.05%-6.29% NaCl equivalent (eqv.) and densities of 0.820-0.935 g/cm³. Laser Raman spectroscopic analyses of the gas phase components of FIs show they are dominated by H₂O, CO₂ and minor amounts of N₂. Fluid inclusions in barite in exhalative-chemical deposit system are only aqueous FIs, homogenization temperature from 105.2 to 157.1 ℃, and salinities of 0.18%-5.55% NaCl eqv. and densities of 0.735-1.173 g/cm³ suggesting from lower ore belt to upper ore belt metallogenic temperature drops, salinities does not change, and the density of fluid increases. Hydrogen and oxygen isotopic study (δ¹⁸O_H₂O: 0.25‰-1.75‰, δD: -103.2‰ to -65.3‰) shows that metallogenic fluid is a mixture of seawater and magmatic water. The predecessors research results of sulfur isotope previous research indicates that the sulfur were provided by magma and bacteria reduction seawater sulfate or basement rock. Lead isotopic compositions of galena show ²⁰⁶Pb/²⁰⁴Pb ratios ranging from 18.449 to 18.519, ²⁰⁷Pb/²⁰⁴Pb ratios from 15.677 to 15.777, and ²⁰⁸Pb/²⁰⁴Pb ratios from 38.875 to 39.145, respectively. Lead isotopes has high radioactive lead isotope compositions with μ values of 9.65~9.80. It suggests that the lead mainly was sourced from crustal components and little from magma. The mixing of ore-forming fluid and seawater is the main metallogenic mechanism of Galonggema deposit.
- Sanjiang metallogenic belt,
- Galonggema,
- ore-forming fluid,
- deposit,
- S isotope,
- Pb isotope,
- H, O isotopes,
- petrology

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沈阳化工大学材料科学与工程学院沈阳 110142

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Fluid Inclusions and H-O-S-Pb Isotope Systematics of the Galonggema Cu Deposit in Yushu, Qinghai Province, China

doi: 10.3799/dqkx.2017.074

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