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祁雨沟金矿区蚀变岩型金矿床是一种由石英脉型矿床向蚀变岩型矿床的过渡类型。金矿体主要由一组北东向蚀变构造破碎带控制，成矿区主要位于北西向古构造与北东向控矿构造的交汇部位。本文根据矿床地质特征，提出了找矿方向及找矿方法。
The altered rock type gold deposit in Qiyuogou gold deposit is a type of transition from quartz vein type ore to altered rock type ore deposit. The gold ore body is controlled mainly by a group of NE-trending alteration tectonic fractures. The metallogenetic area is mainly located at the junction of the NW-trending paleo-structure and NE-trending ore-control structure. Based on the geological characteristics of the deposit, this paper proposed the prospecting direction and prospecting method.