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贵州赋存于沉积岩中的微细浸染型金矿床为低温开放体系中经复杂地质地球化学作用形成。在综合研究该类矿床地质地球化学、矿床组合和元素组合的基础上，拟定实验方案，总结出元素迁移富集的规律。
The finely disseminated gold deposits hosted in Guizhou sediments are formed by complicated geologic geochemical processes in a cold open system. On the basis of comprehensively studying the geogeochemistry, ore deposit composition and elemental combination of this type of deposit, the experimental scheme is drawn up and the law of element migration and enrichment is summarized.