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depth levels of the crust and lithosphere. The mechanisms of the material and structural reconstruction of the Paleozoic basement rocks are ranked as the processes of melange formation, voluminous cataclasis, brittle-plastic flow, and dynamic recrystallization, which had operated during the Alpine tectogenesis. The rock masses of the basement were proved to have experienced significant 3D movements during the platform and orogenic periods of the geologic history of the region discussed. INDEX TERMS: 1033 Geochemistry: Intra-plate processes; 1209 Geodesy and Gravity: Tectonic deformation; 3040 Marine Geology and Geophysics: Plate tectonics; KEYWORDS: geodynamics, orogeny, Tien Shan Region, tectonics.

The Post-Oceanic Geodynamics of the South Tien Shan Region