CAJ | 학술논문

天井山金矿床成矿演化宏观上可分为初始沉积期、构造-岩浆作用预富集期、内生热液富集期和表生风化期，主成矿期内生热液富集期成矿演化在微观上表现为微量金-石英阶段、金-单一硫化物-石英阶段、金-多金属硫化物-石英阶段以及微量金-萤石-方解石-石英阶段。分别对该矿床成矿演化的宏观、微观特征进行分析，并对成矿演化与矿化富集的关系进行探讨，为区内找矿工作提供参考。
천정산금광상성광연화굉관상가분위초시침적기、구조-암장작용예부집기、내생열액부집기화표생풍화기，주성광기내생열액부집기성광연화재미관상표현위미량금-석영계단、금-단일류화물-석영계단、금-다금속류화물-석영계단이급미량금-형석-방해석-석영계단。분별대해광상성광연화적굉관、미관특정진행분석，병대성광연화여광화부집적관계진행탐토，위구내조광공작제공삼고。
Metallogenic evolution of Tianjingshan gold deposit in macroscopic can be divided into initial deposition period,tectonic-magmatic preenrichment period,endogenous hydrothermal enrichment period and supergene weathering period,and in microscopic included trace gold-quartz stage,gold-single sulfide-quartz stage,gold-polymetallic sulphides-quartz stage and trace gold-fluorite-calcite-quartz stage of endogenous hydrothermal enrichment period.The macroscopic and microscopic characteristics of the met-allogenic evolution of Tianjiangshan gold deposit are analyzed in detail,besides that,the relationship be-tween metallogenic evolution and mineralization enrichment is discussed so as to provide reference for the prospecting work in Tianjingshan gold mining area.