辉铋矿
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N a grey mineral consisting of bismuth sulphide in orthorhombic crystalline form. It occurs in veins associated with tin, copper, silver, lead, etc, and is a source of bismuth. Formula: Bi2S3 辉铋矿
Polymetal ore containing bismuth glance, sphalerite and magnetite is rarely seen and typical.
辉铋矿与闪锌矿、磁铁矿共生的多金属矿石较少见，具有一定的典型性。
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