名 称：铜氧化矿石

矿物成分：硫化铜的次生矿物孔雀石为主，伴有黄铁矿、磁黄铁矿、方铅矿。脉石矿物主要为石英、透辉石，有少量透闪石、绿泥石等。

成因类型：海相喷流沉积形成硫化铜矿石后，于地表或近地表矿石中硫化铜经氧化，形成次生矿物孔雀石。

成矿时代：中元古代

主要用途：提取铜的矿石原料。铜用来制造电线、电缆、机电设备。并具有观赏性。

采集地点：内蒙古乌拉特后旗霍格乞铜矿区

Name：Copper Oxide Ore

Mineralogy：Secondary minerals of copper sulfides are dominated by malachite, associated with pyrite, pyrrhotite and galena. Gangue minerals are dominated by quartz, diopside, with subordinate tremolite, chlorite, etc.

Ore genesis：primary sulfides precipitated via submarine exhalation, subsequent elevation resulted in oxidation and precipitation of malachite.

Age：Mesoproterozoic

Usage：material for making electric wire, cable, electric devices.

Sample site：Huogeqi copper mine, Wulatehouqi, Inner Mongolia