引言在帕格-威廉斯矿区的A、B、C三条带中发现了金矿化,Valliant和Bradbrook把这三条带作为一个整体来讨论。“B”带是“A”带的向下延伸部分,这两条带被认为是主要矿带。本文的目的是介绍帕格-威廉斯矿区的地质环境和“A”带金矿体的地质特征。据地下和地表金刚石钻探以及地下和地表的开发和采矿,研究了“A”带。“B”和“C”带也被开发或进行了地质研究。对“B”和“C”带的主要描述,包括对该矿区矿化提供很 Introduction Gold mineralization was discovered in zones A, B and C of the Pug-Williams mine, and Valliant and Bradbrook discuss the three zones as a whole. The “B” zone is the downward extension of the “A” zone, which is considered the major ore zone. The purpose of this paper is to describe the geology of the Pug-Williams mining area and the geological features of the “A” zone gold ore body. According to underground and surface diamond drilling and underground and surface development and mining, studied the “A” belt. The “B” and “C” belts have also been developed or undergone geological studies. The main descriptions of the “B” and “C” bands, including the mineralization provided to the mine area