МАЙКОПСЬКА СЕРІЯ (ОЛІГОЦЕН-НИЖНІЙ МІОЦЕН) СХІДНОГО КАВКАЗУ (АЗЕРБАЙДЖАН): ОСАДКОНАКОПИЧЕННЯ ТА ТЕКТОНІКА

Анотація

Представлено нову геодинамічну модель геологічного розвитку східного сегменту Альпійсько-Гімалайського гірського пасма в межах Азербайджану (східна частина Великого Кавказу, Нижньокуринска западина і Талиш) протягом майкопу.
Вперше складено карти товщин для кожного стратиграфічного підрозділу майкопу, що дозволило встановити наявність великої кількості ділянок з континентальними умовами розвитку.
Проведеними дослідженнями встановлено, що накопичення майкопської товщі відбувалося в шельфовій зоні, в цілому, мілководного басейну, а не глибоководного, як вважалося раніше, аналога сучасних архіпелагових морів, де в протоках між островами відбувалося формування осадового комплексу, переважно глинистими породами дрібнозернистого складу

Ключові слова: майкопська серія, палеобасейн, седиментація, Східний Кавказ, Азербайджан

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