Abstract:

The Wanglingkou gold deposit is a subvolcanic rock type gold deposit. The gold mineralization distributes in the quartz syenite porphyry body of Yanshan Period. The anomaly value is strong in the east of the area, weak in the south, high in the north , low in the south. It has close relationship with cranny and metallization extent. The quartz syenite porphyry body of Yanshan Period is the wall of lode. It is a lso the major metallization matrix rock. In the periphery of the area, there is the resemble and the same metallization geological background and the sign of gold metallization. It shows that the prospect of prospecting the same type of gold deposit is better.

Key words: geological feature, subvolcanic rock, ore-controlling mechanism, Hebei