摘要
The Baishan molybdenum deposit is located in the Sanchakou-Baishan porphyry copper molybdenum ore belt, which belongs to the southeast edge of circum Zhungaer porphyry ore belt. This deposit occurs in the exo contact zone of the granite, which consists of biotite felsic hornfels originated from the Early Carboniferous Gandun Formation. The orebodies occur as veins, lens and layers, 100~3 000 m long, 2~38.4 m thick, with average Mo grade of 0.03%~0.78%. Ore metals consist of mainly molybdenum with accompanying copper, silver, and rhenium. Currently the proven metal Mo reserve is 0.3 M tons. Based on geological, geophysical and geochemical exploration information, the neighboring areas in the south, west and east parts of the current ore zone is promising for further mineral prospecting.