名 称：铜钼矿石 

矿物成分：矿石矿物主要有黄铜矿、辉钼矿，其次有斑铜矿、辉铜矿、黝铜矿、闪锌矿。脉石矿物主要有石英、钾长石、斜长石、绢云母，其次为伊利石、水白云母，少量方解石、金红石、硬石膏、萤石、高岭石、褐帘石等。

成因类型：斑岩型

成矿时代：侏罗纪

主要用途：是提取铜、钼的主要矿石原料。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：内蒙古新巴尔虎右旗乌奴格吐山铜钼矿区

Name：Copper-Molybdenum Ore

Mineralogy：Ore minerals dominated by pyrite, molybdenite, with subordinate bornite, chalcocite, tetrahedrite, and sphalerite. Gangue minerals consist mostly of quartz, potassium feldspar, plagioclase, ande sericite, with subordinate illite, hydromuscovite, and minor amount of calcite, rutile, anhydrite, fluorite, Kaolinite, alunite, etc.

Genesis：Porphyry

Age：Jurassic

Usage：Major source for extracting copper and molybdenum. Copper is mostly used in electric industry, also used in defense , mechine manufacture, organic chemistry, art and crafts, and agriculture. Molybdenum is important raw material for metallurgy, electric industry, chemical industry and aerospace industry.

Sample site：Wunugetushan, Xinbaerhuyouqi, Inner Mongolia.