scholarly journals Corrigendum to “Geochronology and origin of the Sarekoubu gold deposit, southern Altaides, China: Ar-Ar dating of vein quartz and Cu-Zn-Fe isotopes” [Ore Geol. Rev. 124 (2020)103642, 9–10]

2021 ◽  
pp. 104499
Author(s):  
Jiuhua Xu ◽  
Hui Zhang ◽  
Longhua Lin ◽  
Xing Xiao ◽  
Chunjing Bian
Keyword(s):  
Gold Deposit ◽  
Vein Quartz ◽  
Fe Isotopes

Geochronology and origin of the Sarekoubu gold deposit, southern Altaides, China: Ar-Ar dating of vein quartz and Cu-Zn-Fe isotopes

2020 ◽  
Vol 124 ◽  
pp. 103642
Author(s):  
Jiuhua Xu ◽  
Hui Zhang ◽  
Longhua Lin ◽  
Xing Xiao ◽  
Chunjing Bian
Keyword(s):  
Gold Deposit ◽  
Vein Quartz ◽  
Fe Isotopes

The Study of Fluid Inclusions in Haoyaoerhudong Gold Deposit

2013 ◽  
Vol 813 ◽  
pp. 278-280
Author(s):  
De Quan Wang ◽  
Jian Chao Liu ◽  
Hai Dong Zhang ◽  
Li Hong Zheng ◽  
Wen Hui Men
Keyword(s):  
Gold Deposit ◽  
Fluid Inclusions ◽  
Late Stage ◽  
Quartz Vein ◽  
Inner Mongolia ◽  
Fluid Composition ◽  
Vein Quartz ◽  
Sulfide Phase

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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