ДИНАМІКА ГЛЯЦІАЛЬНИХ ПРОЦЕСІВ В ПІЗНЬОМУ ПЛЕЙСТОЦЕН-ГОЛОЦЕНІ В РАЙОНІ АНТАРКТИЧНОГО ПІВОСТРОВА НА ПІДСТАВІ ОПУБЛІКОВАНОЇ ЛІТЕРАТУРИ

Автор(и)

  • Г. С. Педан Одеський національний університет імені І. І. Мечникова, геолого-географічний факультет, кафедра морської геології, гідрогеології, інженерної геології та палеонтології, Україна https://orcid.org/0000-0001-7361-5880
  • Ю. В. Каракича Одеський національний університет імені І. І. Мечникова, геолого-географічний факультет, кафедра морської геології, гідрогеології, інженерної геології та палеонтології, Україна

DOI:

https://doi.org/10.18524/2303-9914.2025.1(46).333957

Ключові слова:

геологічні умови, гляціальні процеси, льодовиковий покрив, Антарктичний півострів, пізній плейстоцен-голоцен

Анотація

В роботі узагальнено результати попередніх вітчизняних і зарубіжних досліджень Антарктичного півострова та району Української антарктичної станції «Академік Вернадський», проведено аналіз опублікованих та електронних матеріалів з інтерпретацію результатів та подальшим їх зіставленням. Використаний комплексний підхід в узагальненні наукової літератури, яка висвітлює гляціальну динаміку та її зв’язок із глобальними кліматичними змінами та умовами осадконакопичення на Антарктичному півострові в пізньоплейстоцен-голоценовий час.

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Опубліковано

2025-06-30

Як цитувати

Педан, Г. С., & Каракича, Ю. В. (2025). ДИНАМІКА ГЛЯЦІАЛЬНИХ ПРОЦЕСІВ В ПІЗНЬОМУ ПЛЕЙСТОЦЕН-ГОЛОЦЕНІ В РАЙОНІ АНТАРКТИЧНОГО ПІВОСТРОВА НА ПІДСТАВІ ОПУБЛІКОВАНОЇ ЛІТЕРАТУРИ. Вісник Одеського національного університету. Географічні та геологічні науки, 30(1(46), 309–322. https://doi.org/10.18524/2303-9914.2025.1(46).333957

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ЗАГАЛЬНА, МОРСЬКА ГЕОЛОГІЯ ТА ПАЛЕОНТОЛОГІЯ