ПИТАННЯ ВИВЧЕННЯ ОСАДОВОГО КОМПЛЕКСУ ЕОЦЕНУ КРИМСЬКОГО І КЕРЧЕНСЬКОГО ПІВОСТРОВІВ
DOI:
https://doi.org/10.30836/igs.2522-9753.2015.145320Ключові слова:
стратиграфія, еоцен, Кримський і Керченський півостровиАнотація
У статті представлена актуалізована стратиграфічна схема еоценових відкладів Кримського і Керченського півостровів за результатами узагальнення та аналізу літолого-палеонтологічної інформації, використання біостратиграфічних розробок за різними групами мікро- і макрофосилій, а також сучасних стратиграфічних уявлень. Дослідження були проведені з дотриманням вимог Стратиграфічного кодексу України (2012 р.). У схемі, що пропонується, прийнята сучасна Міжнародна стратиграфічна шкада (2012-2014 рр.) і модернізована регіональна стратиграфічна шкала палеогену Південної України (2013 р.). Наведена літолого-палеонтологічна характеристика 18 місцевих стратиграфічних підрозділів, які входять до складу бахчисарайського, сімферопольського, новопавлівського, кумського і альмінського регіоярусів (горизонтів). Уточнені стратиграфічний об’єм, поширення та вік описаних світ, товщ, пачок, верств з фауною еоцену Кримського і Керченського півостровів. Шість місцевих стратонів є новими для Рівнинного і передгір’я Криму, Керченського півострова: кишлавська товща (бахчисарайський регіоярус); славутицька світа, вапняки глинисті з дрібними нумулітами і Assilina tenuimarginata (сімферопольський регіоярус); дмитрівська товща (бахчисарайський + сімферопольський регіояруси); мергелі і вапнисті глини з Acarinina rotundimarginata і Globogerinatheka subconglobata (новопалвський + кумський регіояруси); малобабчинська світа (бахчисарайський – альмінський регіояруси).Посилання
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