据作者近年研究结果,地台活化具有重要的成矿作用。这种成矿作用包括两方面:第一是由活化时期的岩浆活动带来的以有色金属及稀有金属为主的内生矿床,第二是在活化进行过程中由于拱曲作用(主要为拗陷,有时兼有或代以断裂)而发生大幅度下陷的凹地,其中沉积作用带来了丰富的外生矿床,主要是(火乚)、油页岩、铁、锰、铝、盐类(石膏、盐)等沉积矿床。这些矿床在特性上完全不同于地槽型或地台型沉积矿 According to the author’s research results in recent years, platform activation has important mineralization. The metallogenesis includes two aspects: the first is the endogenous deposits dominated by the magmatic activity during the activation period, mainly of non-ferrous metals and rare metals; the second is due to the arching during the activation process Subsidence, sometimes subsoil or substitutive faults), and the sedimentation has resulted in abundant exogene deposits, mainly firestones, oil shale, iron, manganese, aluminum and salts Gypsum, salt) and other sedimentary deposits. These deposits are completely different in nature from the geosyncline or platform sediment