Yu Xiangdong, Guo Wenxiu. OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN[J]. Geology and Resources, 1997, 6(2): 114-123.
Citation:
Yu Xiangdong, Guo Wenxiu. OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN[J]. Geology and Resources, 1997, 6(2): 114-123.
Yu Xiangdong, Guo Wenxiu. OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN[J]. Geology and Resources, 1997, 6(2): 114-123.
Citation:
Yu Xiangdong, Guo Wenxiu. OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN[J]. Geology and Resources, 1997, 6(2): 114-123.
OXYGEN, LEAD AND CARBON ISOTOPIC CHARACTERISTICS AND ORE-FORMING FLUIDS OF GOLD DEPOSITS IN WEASTERN HENAN
On the basis of O, Pb and C isotopic studies of many gold deposits in western Henan, The authors suggest that the ore-forming fluid of gold deposits is deep flow. It was formed at great depths during evolution of geology. Mineralization was related to the fluids that flowed from deep to upper and was hybridized by meteoric water.
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