The northwestern Guizhou Province is located in a rift basin with some lead-zinc deposits controlled by the faults and strata.
黔西北地区是一个裂谷盆地构造区，盆地内发育铅锌矿床，矿化受断裂和地层的联合控制。
The ore-hosted strata of Xitieshan lead-zinc ore deposit is located in a limb of a anticline and suffered from deformation partition.
锡铁山大型铅锌矿床含矿岩系的构造格架位于背斜的一翼，普遍遭受变形分解作用。
The abundant pyrrhotine and marmatite in ore showed that the ore-forming temperature was higher than normal strata-bound lead and zinc deposit.
矿石中的磁黄铁矿及铁闪锌矿的大量出现，预示着成矿温度较一般的层控铅锌矿床为高；
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