CAJ | 학술논문

八卦庙金矿床是赋存于热水沉积岩系中，并受二里河—八卦庙脆－韧性剪切带构造控制的大型金矿床，矿体严格产出在2期石英脉中及其附近。通过对矿区内2期石英脉的研究，将成矿期次初步划分为（早期） NW向石英脉成矿期、（晚期） NE 向石英脉成矿期，早期成矿于190～230 Ma，晚期集中在125～130 Ma。综合研究认为，八卦庙金矿床成因类型应为热水沉积－改造型金矿床。
팔괘묘금광상시부존우열수침적암계중，병수이리하—팔괘묘취－인성전절대구조공제적대형금광상，광체엄격산출재2기석영맥중급기부근。통과대광구내2기석영맥적연구，장성광기차초보화분위（조기） NW향석영맥성광기、（만기） NE 향석영맥성광기，조기성광우190～230 Ma，만기집중재125～130 Ma。종합연구인위，팔괘묘금광상성인류형응위열수침적－개조형금광상。
Baguamiao Gold Deposit occurs in the hydrothermal-sedimentary rocks and is a large scale gold de-posit controlled by the Erlihe-Baguamiao brittle-ductile shear zone.The ore output is confined in the two quartz veins and their vicinity strictly.Based on the research of the two quartz veins,the metallogenic stages are classified into NW quartz vein mineralization ( early stage) and NE quartz vein mineralization ( late stage) .The early mineralization was formed between 190-230 Ma,and the late between 125-130 Ma.By analyzing the type of deposit,the paper takes that the Baguamiao is hydrothermal-sedimentary transformation type gold deposit.