本文探讨了酸性岩浆岩的潜在含矿性及形成条件的标志。酸性岩浆岩与大量的内生矿床有关(首先是锡、钨、钼、稀有金属及稀土,有时还有金、铜、多金属、铁及某些其它金属)。在分析形成条件时,特别注意了总结现有的(首先是原始资料)有关成矿介质的显微包裹体(熔体、流体)资料,并将这些资料与天然的和实验的岩石学资料进行了对比。不同地球化学类型的酸性岩浆岩的含矿性标志是不同的。这些类型是:锂氟类型(包括翁岗岩及其成分类似的火山相含黄玉的流纹岩)、标准类型和碱性花岗岩类型。地球化学类型系指一组化学成分及矿物成分、造岩元素和稀有元素分布 This article explores the potential mineralization of acidic magmatic rocks and the formation of the conditions. Acidic magmatic rocks are associated with a large number of endogenic deposits (above all tin, tungsten, molybdenum, rare metals and rare earths, and sometimes gold, copper, polymetallic, iron and some other metals). In analyzing the formation conditions, particular attention was paid to summarizing existing (primarily raw) data on microscopic inclusions (melt, fluid) related to metallogenic media and making these data in combination with natural and experimental petrological data Contrast. The ore-bearing signs of acidic magmatic rocks of different geochemical types are different. These types are: Lithium Fluoride types (including Wengang Rock and its volcano-associated topaz containing rhyolite), standard types and alkaline granite types. Geochemical type refers to a group of chemical composition and mineral composition, rock-forming elements and rare elemental distribution