摘要
Yantonglazi deposit is one of the newly discovered Ni-Cu-PGE sulfide deposits in eastern Jilin Province, and its characteristics are seldom mentioned at home and abroad. The authors analyzed geological features, mineralogy, chalcography, and electron probe of Yantonglazi PGE-Cu deposit, the results indicate that 1) the orebody occurs mainly in the inner contact belt between gabbro and the epi-metamorphic rock of Wudaogou Group; and 2) the wall rock is the garnetized gabbro formed by hydrothermal metasomatism. This paper comes to a conclusion that the hydrothermal metasomatism is a crucial factor for metallization.