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对内蒙古额仁陶勒盖银矿床主要载银矿物和银矿物的矿物学地球化学特征研究表明：矿床形成与岩浆活动关系密切，成矿流体主要为岩浆热液，属典型的中低温岩浆热液矿床。银的赋存状态主要为独立银矿物，它们以包体、显微包体的形式存在于脉石矿物中。在锰银型矿石中，少量银以离子吸附状态存在。系统地划分了银矿物的８种成份系列，为矿山开采和选冶提供了依据。
The study on the mineralogical and geochemical characteristics of the silver-bearing minerals and silver minerals in the Neorengren Tolgoi silver deposit in Inner Mongolia shows that the mineralization is closely related to the magmatic activity. The ore-forming fluids are mainly magmatic hydrothermal fluids, belonging to the typical mid-low temperature magmatic hydrothermal fluid Deposits. The occurrence of silver is mainly independent silver minerals, which are in the form of inclusions and microscopic inclusions in gangue minerals. In manganese silver ore, a small amount of silver exists in an ion-adsorbed state. Systematically divided the silver mineral eight kinds of components of the series, for mining and mineral processing provided the basis.