近几年吉林槽区陆续发现多处不同类型的钼矿床(点)，其主要类型有斑岩型、石英脉型、矽卡岩型、破碎蚀变岩型。
In recent years, there more different types mo deposits (spots) have been discovered in Jilin geosynclinal area, mainly porphyry, quartz vein, skarn and fracture altered rock deposits.
论述了矽卡岩一斑岩型钼矿床的成矿地质条件、围岩蚀变、矿床特征和矿床成因。
Furtherly are discussed geological condition under which skarn - porphyritic molybdenum ore deposit are formed, alterations in wall rocks and the genesis of the Mo-deposit.
河南栾川南泥湖钼矿田属东秦岭-大别山钼成矿带的重要组成部分，矿田内矽卡岩- 斑岩型钼矿床的成矿物质赋存状态具有区域代表性。
Nannihu molybdenum mine field is the important component part of the East Qinling-dabie mountain ore forming belt, in which the ore-forming material occurrence state of s…
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