导论金矿出现在加拿大地盾的许多绿岩带中,具有多种地质环境并可被划分成许多矿床类型,包括最近在赫姆洛发现的类型。研究者对金矿的生成是受地层和构造控制已开展争论。赫姆洛的威廉斯矿区的帕格-威廉斯金矿包括A、B、C三带。三个地貌上各异的金矿,均赋存在独特的断层控制的地层层序中,其规模、岩石、构造、丰度、含金的 Introduction Gold occurs in many of the greenstone belts of the Canadian Shield, has a variety of geological settings and can be divided into many deposit types, including those recently discovered in Hemlo. Researchers have controversy over the formation of the gold mine, which is controlled by the strata and tectonics. The Pugley-Williams Gold Mine in the Humble Mine of Williams includes the A, B, and C belts. The three gold deposits with different topographies all belong to the unique stratigraphic sequence controlled by faults. Their size, rock, structure, abundance, gold-bearing