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锡霍特中生代褶皱系可分为三段:(1)巴贾尔—下阿穆尔;(2)中段;(3)滨海段。在锡霍特的剖面上,可分出三套地层构成组合。它们是:(1)基底组合;(2)主褶皱组合;(3)非褶皱组合。基底组合由元古代(?)的变质岩系组成,主褶皱组合由从中古生界到早白垩世的地层组成。在有些带,主褶皱组合含有侏罗纪到早白垩世的混杂岩和较老的滑塌层。锡霍特地区的地质发展史中的一个显著特点是自晚古生代以来活动大陆边缘体制多次出现。
The Sikhote Mesozoic fold system can be divided into three sections: (1) Bajar-Amur; (2) Middle section; (3) Coastal section. In the section of Sikhute, three sets of strata can be separated. They are: (1) Substrate combinations; (2) Main fold combinations; (3) Non-fold combinations. The basement assemblage consists of metamorphic metamorphic rocks of the Proterozoic (?) And the main fold assemblage consists of formations from Mesozoic to Early Cretaceous. In some belts, the main fold assemblage contains Jurassic to Early Cretaceous melange and older slippery layers. One of the salient features in the history of the Sithot region’s geological history is the multiple occurrences of the active continental margin system since the Late Paleozoic.