The Study of Fluid Inclusions in Haoyaoerhudong Gold Deposit

De Quan Wang; Jian Chao Liu; Hai Dong Zhang; Li Hong Zheng; Wen Hui Men

doi:10.4028/www.scientific.net/AMR.813.278

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HomeAdvanced Materials ResearchAdvanced Materials Research Vol. 813The Study of Fluid Inclusions in Haoyaoerhudong...

The Study of Fluid Inclusions in Haoyaoerhudong Gold Deposit

Abstract:

Haoyaoerhudong gold deposit is located in Inner Mongolia Wulate county. We analysis the characteristics of fluid composition. Salinity values range is from 3.40% to 20.40%; The density of the fluid is from 0.68 to 0.97 g/cm3;Ore-forming pressure is from 11.44 to 58.42MPa;According them, We can separate the fluid into Quartz-pyrite stage, Ore-forming fluid is divided into four stages in Haoyaoerhudong gold deposit. It is quartz calcite phase, the late stage of quartz vein, quartz polymetallic sulfide phase and quartz Pyrite phase. Quartz polymetallic sulfide phase and quartz Pyrite phase is the main metallogenic period in Haoyaoerhudong gold deposit.

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Periodical:

Advanced Materials Research (Volume 813)

Pages:

278-280

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.813.278

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Online since:

September 2013

Authors:

De Quan Wang, Jian Chao Liu, Hai Dong Zhang, Li Hong Zheng, Wen Hui Men

Keywords:

Density, Haoyaoerhudong Gold Deposit, Ore-Forming Pressure, Salinity

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