2012Geology of AnhuiRequires access

ORE CONTROL FACTORS ANALYSIS AND ORE PROSPECTING DIRECTION PROGNOSIS FOR THE YAOJIALING ORE DEPOSIT

Changsheng Han

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Abstract

The Yaojialing zinc-gold polymetallic ore deposit is a very large one of its type discovered in the Tongling mining camp by No.812 Geological Team during the 10th to 11th Five-Year Plan period.It formed in late Yanshanian period and occurred in limestone xenolith cluster(zone) hosted in the Yaojialing granodiorite porphyry intrusion.The ore body is veinlike,quasi-bedded,lenticular within the upper and lower contact zones and fractured zone of xenoliths.It is mid-low temperature hydrothermal zinc-gold polymetallic ore deposit controlled by deep fault.

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What this paper is about

The Yaojialing zinc-gold polymetallic ore deposit is a very large one of its type discovered in the Tongling mining camp by No.812 Geological Team during the 10th to 11th Five-Year Plan period.It formed in late Yanshanian period and occurred in limestone xenolith cluster(zone) hosted in the Yaojialing granodiorite porphyry intrusion.The ore body is veinlike,quasi-bedded,lenticular within the upper and lower contact zones and fractured zone of xenoliths.It is mid-low temperature hydrothermal zinc-gold polymetallic ore deposit controlled by deep fault.

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Available abstract

The Yaojialing zinc-gold polymetallic ore deposit is a very large one of its type discovered in the Tongling mining camp by No.812 Geological Team during the 10th to 11th Five-Year Plan period.It formed in late Yanshanian period and occurred in limestone xenolith cluster(zone) hosted in the Yaojialing granodiorite porphyry intrusion.The ore body is veinlike,quasi-bedded,lenticular within the upper and lower contact zones and fractured zone of xenoliths.It is mid-low temperature hydrothermal zinc-gold polymetallic ore deposit controlled by deep fault.

Key concepts: Prospecting, Geology, Polymetallic replacement deposit, Geochemistry, Intrusion, Hydrothermal circulation, Xenolith, Gold ore

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