银子坛墓地是贵州黔西北地区一处战国至东汉初期的遗存。
The Yinzitan cemetery, from the warring states period to the beginning of Donghan dynasty is in northwest Guizhou.
本文通过成矿地质背景和成矿规律分析，认为黔西北地区铅锌矿属沉积改造型铅锌矿床。
In this paper, by analyses the metallogenic regulation and metallogenic geologic background, it thought the lead-zinc deposit in northwest Guizhou belong to depositing-reworking lead-zinc deposit.
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 northwestern Guizhou Province is located in a rift basin with some lead-zinc deposits controlled by the faults and strata.
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