斑铜矿是铜和铁的硫化物矿物,含铜量 63.3%斑铜矿,提炼铜的主要矿物原料之一。为等轴晶系,其高温变体为等轴晶系,称等轴斑铜矿。表面易氧化呈蓝紫斑状的锖色,因而得名。新鲜断面呈暗铜红色,金属光泽,莫氏硬度 3,比重4.9~5.0。常呈致密块状或分散粒状见于各种类型的铜矿床中,并常与黄铜矿共生。也形成于铜矿床的次生富集带,但不稳定,而被次生辉铜矿和铜蓝置换。在地表易风化成孔雀石和蓝铜矿。中国云南东川等铜矿床中有大量的斑铜矿。世界代表性产地是美国蒙大那州的比尤特,墨西哥卡纳内阿和智利丘基卡马塔等。
n. bornite ; phillipsite ; erubescite
misc. poikilite
层状主矿体中金主要以细小的自然金形式包裹于斑铜矿和黝铜矿中。
Gold in strati form major orebody is mainly included in bornite and tetrahedrite as fine grain of native gold.
层状主矿体中金主要以细小的自然金形式包裹于斑铜矿和黝铜矿中。
Gold in stratiform major orebody is mainly included in bornite and tetrahedrite as fine grain of native gold.
矿石主要含铜矿物为孔雀石、硅孔雀石,少量的黄铜矿、辉铜矿及极少量的斑铜矿和铜蓝等。
The main copper minerals are malachite, chrysocolla, little chalcopyrite, chalcosine and even little bornite and covellite.
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