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阿尔丹一斯塔诺夫地区是苏联最大的早前寒武纪地层出露地区之一。这套地层可以划分为阿尔丹和斯塔诺夫两个褶皱系,二者在构造面貌、变质作用级别等方面均有差异。迄今对二者的关系知道很少,故以构造—变质面貌将二者彼此分开。然而地学界多认为它们属太古界无疑。因此,整个地区应是一个太古代固结区。在早、中元古代时期,该区破裂为一个被缝合槽分隔的断块系。晚元古代时期,处于地台快速发育阶段。随后在古、中、新生代时期经受了各种构造、岩浆活化作用的干挠。
The Altdin-Stanov region is one of the largest areas exposed by the Precambrian strata in the Soviet Union. This set of strata can be divided into two fold systems of Ardyn and Stanov, both of which have differences in tectonic features and metamorphic levels. So far the relationship between the two know very little, so the tectono-metamorphic face of the two separated from each other. However, many scholars think they belong to the Archeology undoubtedly. Therefore, the entire area should be an Archean Consolidation Zone. In the early and Middle Proterozoic years, the area ruptured into a fault block separated by suture troughs. Late Proterozoic period, in the stage of rapid development platform. Later in the Paleozoic, Mesozoic and Cenozoic period experienced various structures, magmatic activation of the dry scratch.