摘要
巧家县坝统铅锌矿矿体呈脉状、似层状,沿断层破碎带产出,矿体的形态与分布明显受F1断裂构造的控制,矿体围岩为碎裂状白云岩;矿床成因属产于碳酸盐岩中断裂破碎带控制的热液充填-交代脉状矿床。
The ore body of Batong Pb-Zn deposit in Qiaojia is veined,stratoid,in fault fracture zone. The form and distribution of ore body are controlled clear by fault F1. The wall rock of ore body is the fractured dolomitite. It belongs to the hydrothermal filling metasomatic deposit controlled by fault fracture zone in carbonate rock in genesis.
引文
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