摘要
Through the analysis of metallogenetic geological conditions,the formation of Liudiangou silver deposit in Horqin Right Front Banner of the Inner Mongolia related to the Late Jurassic continental facies intermediate acidity volcanic rock and the Early Cretaceous biotitic granodiorite porphyry,pyritized granodiorite porphyry.The NE,NW direction structures are the main ore-control structures in the region,the former is ore-bringing structure,the latter is host structure,therefore,strata,magmatic rocks,structures of "the Trinity" ore-controlling are ore-control regularity in this area.The metallogentic epoch is the late stage of the Early Cretaceous.Genetic type is a magmatic hydrothermal type.