ПІЗНЬОМІОЦЕН-ПЛІОЦЕНОВІ ТЕРАСИ ПІВНІЧНОУКРАЇНСЬКОЇ ПАЛЕОСЕДИМЕНТАЦІЙНОЇ ПРОВІНЦІЇ. Стаття 2. Алювіально-озерне походження неогенових терасових рівнів

Автор(и)

  • A. Karpenko Інститут геологічних наук НАН України, Київ, Ukraine

DOI:

https://doi.org/10.30836/igs.1025-6814.2018.1.126442

Ключові слова:

Неоген, терасові рівні, алювіально-озерні відклади

Анотація

Обгрунтовано погляд на походження неогенових терас Дніпровсько-Донецької западини як денудаційно-алювіально-озерно-акумулятивне

Посилання

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