


钼矿石
名 称:钼矿石
矿物成分:矿石矿物主要为辉钼矿,可见方铅矿、闪锌矿、黄铜矿、黄铁矿;脉石矿物主要为石英、绿泥石、绢云母、方解石及萤石等。
成因类型:热液型
成矿时代:中生代
主要用途:提取钼的主要矿石原料。金属钼是冶金、电气、化工、航空和航天等制造业中不可缺少的原料。钼在冶金工业上,用作生产各种合金钢的添加剂,并能与钨、镍、钴、锆、钛等组成高级合金。金属钼大量用作高温电炉的发热材料和结构材料,因钼的热中子俘获截面小、具高持久强度,还可用作核反应堆的结构材料。
采集地点:内蒙古巴林左旗二道营子钼矿区
Name:Molybdenum Ore
Mineralogy:Ore minerals dominated by molybdenite, with visible galena, sphalerite, chalcopyrite and pyrite. Gangue minerals consist mostly of quartz, chlorite, sericite, calcite and fluorite.
Ore genesis:Hydrothermal
Age:Mesozoic
Usage:Major source for extracting molybdenum. Molybdenum is essential raw material for metallurgy, electric industry, aero and space industry. In metallurgy molybdenum is used for making alloys, combined with tungsten, nickel, cobalt, zirconium, titanium, etc. Molybdenum is also used as exothermic and structural material in high temperature electric furnace. As molybdenum has small truncated area of thermal neutron capture and long lasting strength, it could be used in nuclear reactor as structural material.
Sample site:Erdaoyingzi, Balinzuoqi, Inner Mongolia