2003Journal of East China Geological InstituteRequires access

Fluid Inclusion Study on the Yangshan gold deposit, south Gansu,China

Zhao Bai-shen

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Abstract

Yangshan gold deposit is a supper large gold deposit occur in Devonian epimetamorphised, phyllite or limestone, found by gold geological party of CAPF in recent years. In this paper, based on the studies of fluid inclusions trapped in quartzes and calcites, the ore-forming fluid characteristics are described, and the ore genesis of this deposit is revealed.

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Yangshan gold deposit is a supper large gold deposit occur in Devonian epimetamorphised, phyllite or limestone, found by gold geological party of CAPF in recent years. In this paper, based on the studies of fluid inclusions trapped in quartzes and calcites, the ore-forming fluid characteristics are described, and the ore genesis of this deposit is revealed.

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Available abstract

Yangshan gold deposit is a supper large gold deposit occur in Devonian epimetamorphised, phyllite or limestone, found by gold geological party of CAPF in recent years. In this paper, based on the studies of fluid inclusions trapped in quartzes and calcites, the ore-forming fluid characteristics are described, and the ore genesis of this deposit is revealed.

Key concepts: Phyllite, Geology, Geochemistry, Devonian, Fluid inclusions, Inclusion (mineral), Mineralogy, Mining engineering

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