Abstract

Stratigraphic scheme of the division (at the level of formation) of Triassic to Neogene deposits of the central part of Crimea based upon generalizations of our own results and analysis of published and unpublished data was proposed.

Highlights

  • of Triassic to Neogene deposits of the central part of Crimea based upon generalizations of our own results and analysis

  • Nikishin A.M., Ziegler P.A., Panov D.I. et al Mesozoic and Cenozoic evolution of the Scythian Platform-Black Sea-Caucasus domain // Peri-Tethys Mem. 6

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Summary

НИЖНИЙ И СРЕДНИЙ ПОДЪЯРУСЫ

ПОДЪЯРУС — АПТСКИЙ ЯРУС K1bs+kz — биасалинская и коясджилдинская свиты объединенные. ВЕРХНИЙ ПОДЪЯРУС — АПТСКИЙ ЯРУС K1an+ms — ангарская и малосалгирская толщи объединенные. СРЕДНИЙ И ВЕРХНИЙ ПОДЪЯРУСЫ — ГОТЕРИВСКИЙ ЯРУС. НИЖНИЙ ПОДЪЯРУС K1tk+bj —таскаринская и биюкянкойская толщи объединенные. СРЕДНИЙ И ВЕРХНИЙ ПОДЪЯРУС — ГОТЕРИВСКИЙ ЯРУС. НИЖНИЙ ПОДЪЯРУС K1mž+sv — межигирская и соловьевская толщи объединенные

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