从岩石圈板块构造立场解释了俄罗斯远东地区南部的地质构造与演化。同时指出在构造形成过程中，中生代大洋岩石圈板块向欧亚大陆的俯冲起了主导作用。特别注意到活动性大陆边缘，沿其形成了弧前盆地和增生楔。划分出二类增生杂岩：鳞片状推覆体和混杂岩。在中生代不同年龄的杂岩中占主导地位的两者之一，可见侧向分带。在演化的较晚阶段，构造主要被脆性及韧性走滑位移所复杂化。 From the tectonic standpoint of the lithosphere, it explains the geological structure and evolution in the southern Far East of Russia. At the same time, it is pointed out that the Mesozoic oceanic lithospheric plate played a leading role in the subduction of Eurasia during the tectonic process. Special attention was drawn to the active continental margin along which pre-arcuate basins and accretionary wedges formed. Divided into two types of accretionary complex: scaly nappe and melange. One of the dominant dykes in the Mesozoic age complex shows lateral zonation. At later stages of evolution, the structure is mainly complicated by brittle and ductile strike-slip displacements.