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矿床属热液充填交代类型,产于近某大断裂两侧的大理岩中,或远离某断裂的黑云母大理岩与其它岩层接触带上、金矿体呈脉状,有两种类型:一是黄铁、磁铁矿型金矿,含金较高,可达独立工业矿体;另一种是伴生在铅锌矿中的金矿,金只作伴生元素利用。两种类型的金矿均含银。矿石为块状和浸染状。沿某断裂两侧40Km~2范围内有八个规模较大的矿体群,可能发展成为中型以上规模的金、银、铅、锌等综合矿床。
The deposit belongs to the hydrothermal filling metasomatism type and is produced in marble near both sides of a large fault or away from the contact zone between a fractured biotite marble and other strata. There are two types of gold ore bodies: one Is pyrite, magnetite type of gold, high gold, up to independent industrial ore body; the other is associated with lead-zinc mine gold, gold only for the use of associated elements. Both types of gold contain silver. The ore is massive and disseminated. There are eight large ore body groups within 40Km ~ 2 on both sides of a fault, and may develop into a comprehensive deposit of gold, silver, lead and zinc above the medium size.