众所周知,在苏联境内金矿化的地球动力学状态与四类地区有关,即:地台、优地槽和冒地槽发育区、构造-岩浆活动区。对含金区域地壳深部构造研究所获得的资料,常与经典的(地槽的)概念不太相符,这就需要对一系列原理和观点重新审定。特别是有可能划分出作为主要构造单元的中央岩块——微大陆,在那里裂谷作用和随后的水平移位决定了内生金矿化的部位。人们已经确定了大陆与大洋交界的边缘火山带、内陆带以及岛弧与特殊金矿 It is well known that the geodynamic status of gold mineralization in the Soviet Union is related to four types of areas, namely, the platform, the gnarl trough and the gorges trough development zone and the tectono-magmatic activity zone. The information obtained from the study of the deep crustal structure in the gold-bearing region often does not quite match the classical concept of the trough, which requires a series of revisions to the principles and perspectives. In particular, it is possible to classify the central rock mass as the main tectonic unit - the micro-continent, where rifting and subsequent horizontal displacement determine the site of endogenous gold mineralization. People have identified the marginal volcano, continental belt and island arc with the special gold mine