冷水北沟铅锌矿赋存于元古界栾川群和管道口群地层中，矿体受断裂破碎带及矽卡岩带控制。
The Lenshuibeigou lead-zinc deposit occurs in Proterozoic Luanchuan group and Guandaokou group formation and is controlled by faulted and fractured zone and skarn zone.
矿床应属矽卡岩型铅-锌矿床。
Therefore the deposit belongs to skarn type of lead and zinc deposit.
大桥磁铁硫化物型铅锌矿床是一新的矿化类型，可细分为磁铁硫化物和层状矽卡岩两种亚型。
The Daqiao magnetite-sulfide type Ph-Zn deposit, which is a new Ph-Zn type, can be subdivided two series: magnetite-sulfide and banded skarn.
大桥磁铁硫化物型铅锌矿床是一新的矿化类型，可细分为磁铁硫化物和层状矽卡岩两种亚型。
The Daqiao magnetite-sulfide type Ph-Zn deposit, which is a new Ph-Zn type, can be subdivided two series: magnetite-sulfide and banded skarn.
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