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Fluid Inclusion Geochemistry of Metallic Ore Deposits in the South‐Central Sector of the Da Hinggan Mountains in China

Fluid Inclusion Geochemistry of Metallic Ore Deposits in the South‐Central Sector of the Da... Abstract: Physicochemical parameters of mineralization such as temperature, pressure, salinity, density, composition and boiling of ore fluids as well as pH, Eh, fo2 and reducing parameter in the process of mineralization of major ore deposits in the study district have been obtained by the authors through systematic observation and determination of characteristics and phase changes of fluid inclusions at different temperatures and analysis of gaseous and liquid phase compositions of the inclusions, thus providing a scientific basis for the division of mineralization‐alteration stages, types of mineral deposits and minerogenetic series and the deepening of the knowledge about the ore‐forming processes and mechanisms of mineral deposits. It is indicated that the deposits of the same type have similar fluid inclusion geochemical features and physicochemical parameters though they belong to different minerogenetic series, while the compositions of inclusions are not conditioned by deposit types but closely related to the minerogenetic series of deposits. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta Geologica Sinica (English Edition) Wiley

Fluid Inclusion Geochemistry of Metallic Ore Deposits in the South‐Central Sector of the Da Hinggan Mountains in China

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References (4)

Publisher
Wiley
Copyright
© 1995 Geological Society of China
ISSN
1000-9515
eISSN
1755-6724
DOI
10.1111/j.1755-6724.1995.mp8003005.x
Publisher site
See Article on Publisher Site

Abstract

Abstract: Physicochemical parameters of mineralization such as temperature, pressure, salinity, density, composition and boiling of ore fluids as well as pH, Eh, fo2 and reducing parameter in the process of mineralization of major ore deposits in the study district have been obtained by the authors through systematic observation and determination of characteristics and phase changes of fluid inclusions at different temperatures and analysis of gaseous and liquid phase compositions of the inclusions, thus providing a scientific basis for the division of mineralization‐alteration stages, types of mineral deposits and minerogenetic series and the deepening of the knowledge about the ore‐forming processes and mechanisms of mineral deposits. It is indicated that the deposits of the same type have similar fluid inclusion geochemical features and physicochemical parameters though they belong to different minerogenetic series, while the compositions of inclusions are not conditioned by deposit types but closely related to the minerogenetic series of deposits.

Journal

Acta Geologica Sinica (English Edition)Wiley

Published: Sep 1, 1995

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