


钼矿石
名 称:钼矿石
矿物成分:矿石矿物主要为辉钼矿、黄铜矿,其次有斑铜矿、闪锌矿、方铅矿等。脉石矿物主要为石英、角闪石、透闪石等,少量的方解石、长石、阳起石等。
成因类型:斑岩型
形成时代:早白垩世
主要用途:主要是提炼金属钼、铜的主要矿石原料。铜在电气工业中用量最大;同时在国防、机械制造、有机化工及工艺美术、农业中均有使用。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。
采集地点:内蒙古阿鲁科尔沁旗敖伦花铜钼矿区
Name:Molybdenum Ore
Mineralogy:Ore minerals dominated by molybdenite and chalcopyrite, with subordinate bornite, sphalerite and galena. Gangue minerals consist mostly of quartz, amphibole and tremolite, with minor calcite, feldspar and actinolite.
Ore genesis:Porphyry type
Age:Early Cretaceous.
Usage:Major source for extracting molybdenum and copper. Copper is mostly used in electronic industry, also used in defense industry, machinery manufacture, organic chemistry aero and space industry, metallurgy, and arts and crafts.
Sample site:Aolunhua Copper-molybdenum Mine, Alukeerqin, Inner Mongolia