Tabiiy fanlar

ГЕОДИНАМИКА ЮРСКО-ПАЛЕОЗОЙСКИХ СТРУКТУРНЫХ ПЛАНОВ ЗОНЫ СОЧЛЕНЕНИЯ СУДОЧЬЕГО ПАЛЕОПРОГИБА И БЕРДАХСКОГО ВАЛА

tectonics, lithology, stratigraphy, paleorift system, Sudochi paleotrough, deposits, structure, genetic type, Lower Jurassic interval.

Authors

This article examines the tectonics, lithology, and stratigraphy of sediments in the Sudoch paleo-trough zone of the Berdakh-Takhtakair paleorift system. Deep-sunk Lower and Middle Jurassic sediments within the paleorift system are studied. It has been established that the Berdakh-Takhtakair swell is 800–1000 m higher than the central part of the Sudochi Trough.