Mantle source and magma oxygen fugacity of Permian Ni Cu sulfide-bearing mafic-ultramafic intrusions in the Inner Mongolia, North China: Controls on the sulfide saturation of magmas in the Andean-style continental convergent margins

Lithos ◽  
2021 ◽  
pp. 106105
Author(s):  
Yonghua Cao ◽  
Christina Yan Wang ◽  
Bo Wei ◽  
Hongtian Bao
Keyword(s):  
Oxygen Fugacity ◽  
Mantle Source ◽  
Inner Mongolia ◽  
North China ◽  
Convergent Margins ◽  
Sulfide Saturation

scholarly journals Re-Discussion on the Metallogenic Age of the Hadamengou Gold Deposit in Inner Mongolia, China

2016 ◽  
Vol 5 (2) ◽  
pp. 85
Author(s):  
Yu Zhang ◽  
Yangyang Chen
Keyword(s):  
Gold Deposit ◽  
Inner Mongolia ◽  
North China ◽  
Northern Margin ◽  
The North ◽  
Geological Evolution ◽  
Western Segment ◽  
Mineralization Age ◽  
Extensive Collection ◽  
Metallogenic Age

The Hadamengou gold deposit is located in the western segment of the northern margin of the North China Craton (NCC). The mineralization age of the Hadamengou gold deposit is a matter of controversy. Based on the extensive collection the results of previous research, we infer that the Hadamengou gold deposit is exposed to prolonged geological evolution. It was formed as early as the Middle Hercynian orogen. The metallization mainly took place in the Early Indosinian epoch.

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