大兴安岭岔路口斑岩钼矿床流体成分及成矿意义

熊索菲; 何谋惷; 姚书振; 崔玉宝; 胡新露; 陈斌

doi:10.3799/dqkx.2014.077

Volume 39 Issue 7

Jul. 2014

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Xiong Suofei, He Mouchun, Yao Shuzhen, Cui Yubao, Hu Xinlu, Chen Bin, 2014. Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis. Earth Science, 39(7): 820-836. doi: 10.3799/dqkx.2014.077

Citation:

Xiong Suofei, He Mouchun, Yao Shuzhen, Cui Yubao, Hu Xinlu, Chen Bin, 2014. Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis. Earth Science, 39(7): 820-836. doi: 10.3799/dqkx.2014.077

Citation:

Xiong Suofei, He Mouchun, Yao Shuzhen, Cui Yubao, Hu Xinlu, Chen Bin, 2014. Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis. Earth Science, 39(7): 820-836. doi: 10.3799/dqkx.2014.077

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Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis

doi: 10.3799/dqkx.2014.077

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
3.
Regional Geological Institute of Shaanxi Bureau of Geology and Mineral Resources, Xianyang 712000, China

Received Date: 2013-10-12
Publish Date: 2014-07-15

Abstract

Abstract

The Chalukou Mo deposit lies in the northern Great Xing'an Range, in which veinlet and breccia dominate mineralization. The whole hydrothermal ore-forming processes involve the following four stages: I. quartz-potash feldspar stage; II. quartz-molybdenite stage; III. quartz-polymetallic sulfide stage; IV. quartz-fluorite-calcite stage. The petrographic and laser Raman spectroscopy study show that the melt-fluid inclusions in quartz phenocryst contain component of oligoclase and albite, indicating they directly exsolved from primary magma. Halite, sylvite, hematite, and gypsum are recognized as daughter minerals in S-type inclusions of granite porphyry, suggesting high oxygen fugacity. The stageⅠquartz captures (L+V)-type, C-type, and S-type (contain halite, sylvite, hematite, and anhydrite daughter minerals) fluid inclusions. The stage Ⅱ quartz captures (L+V)-type, C-type, and S-type (contain halite, sylvite, chalcopyrite, and molybdenite daughter minerals) fluid inclusions, in addition, V-type and S-type fluid inclusions are coexistent. In the stage III, there are (L+V)-type and S-type with calcite as daughter minerals. Stage IV develops (L+V)-type and L-type fluid inclusions. Microthermometric data show the homogenization temperatures (530 ℃→120 ℃) and salinities (66.7% NaCl equiv→1.2% NaCl equiv) decrease gradually. The gas components have a certain amount of CO₂ in every stage, and the liquid components in fluid inclusions have Na⁺, K⁺, Ca²⁺, Cl^-, and SO₄^2-, and small amount of F^-. The initial fluids are high oxygen fugacity and salinity NaCl-H₂O-CO₂ fluid system with abundant CO₂. The homogenization temperatures, salinities, lgf_O₂, and CO₂ content tend to fall from the early to late stage. The decline of homogenization temperatures, salinities, and CO₂ content as well as sericitization greatly hinder the depositing of metallogenic elements.
- ore-forming fluid,
- fluid inclusion,
- porphyry molybdenum deposit,
- Chalukou,
- geochemistry

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References(79)

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Compositions and Microthermometry of Fluid Inclusions of Chalukou Porphyry Mo Deposit from Great Xing'an Range: Implications for Ore Genesis

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