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PRELIMINARY DISCUSSION ON THE GENESIS AND GEOLOGI CAL CHARACTERISTICS OF ASHALE GOLD DEPOSIT

Yang Ze

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Abstract

The Ashale gold deposit is produced in the argillaceous limestone and sand conglomarate of Hudukedaban Formation of Upper Ordovician,which belongs to the external contacting belt of Early Variscan granodiorite.It is controlled by the fault belt.It waves weekly and is widden or narrowed partly.There is an orogenic belt on the ground and in the lower part.The source rock of metallogy and hosting rock are related to the granodiorite.It belongs to a skarn gold deposit.

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What this paper is about

The Ashale gold deposit is produced in the argillaceous limestone and sand conglomarate of Hudukedaban Formation of Upper Ordovician,which belongs to the external contacting belt of Early Variscan granodiorite.It is controlled by the fault belt.It waves weekly and is widden or narrowed partly.There is an orogenic belt on the ground and in the lower part.The source rock of metallogy and hosting rock are related to the granodiorite.It belongs to a skarn gold deposit.

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Available abstract

The Ashale gold deposit is produced in the argillaceous limestone and sand conglomarate of Hudukedaban Formation of Upper Ordovician,which belongs to the external contacting belt of Early Variscan granodiorite.It is controlled by the fault belt.It waves weekly and is widden or narrowed partly.There is an orogenic belt on the ground and in the lower part.The source rock of metallogy and hosting rock are related to the granodiorite.It belongs to a skarn gold deposit.

Key concepts: Geology, Skarn, Ordovician, Geochemistry, Fault (geology), Mining engineering, Seismology, Petrology

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