СТРАТИГРАФІЧНА СХЕМА НЕОГЕНОВИХ ВІДКЛАДІВ КРИМСЬКОГО ПІВОСТРОВА

Yu.V. Vernyhorova


DOI: http://dx.doi.org/10.15421/121606

Анотація


За результатами власних досліджень та узагальнення наукових даних у численних публікаціях та геологічних звітах про літо- та біофаціальні особливості неогенових відкладів Кримського півострова проведено ревізію існуючих стратиграфічних схем (1993; 1995 – рукопис; 1996 – рукопис) та легенд до Державних геологічних карт (2004, 2006-2008) і, як результат, запропоновано нову модернізовану стратиграфічну схему. Під час цих досліджень здійснено переінтерпретацію віку окремих стратиграфічних рівнів, уточнено стратиграфічні об’єми для деяких місцевих стратонів попередніх стратиграфічних схем, переглянуто їх стратиграфічний статус і відредаговано назви (згідно із Стратиграфічним кодексом України, 2012). За єдністю літологічних ознак та біостратиграфічних характеристик неогенові відклади півострова, за необхідністю, об’єднано у нові місцеві стратиграфічні підрозділи (світи, верстви, товщі). При виділенні місцевих стратонів на Кримському півострові враховано єдність їх літофаціальних характеристик і видового розмаїття палеонтологічних решток з одновіковими відкладами прилеглих територій Північного Причорномор’я та Керченського півострова. За наявності характерного комплексу органічних решток у складі деяких місцевих стратонів виділено біостратиграфічні підрозділи – «верстви з фауною». За керівними видами різних палеонтологічних груп обґрунтовано вік виділених місцевих ст ратиграфічних підрозділів. Проведено кореляцію цих стратонів із регіоярусами неогену Східного Паратетісу.

Ключові слова


світа; верстви; товща; структурно-фаціальна зона; стратиграфія; неоген; Кримський півострів; Південь України; Східний Паратетис

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Посилання


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DOI: http://dx.doi.org/10.15421/121606


Адреса редколегії: м. Дніпропетровськ, пр. Карла Маркса, 36, к.2, ДНУ імені Олеся Гончара, НДІ геології, Україна, 49044

E-mail: stefanskyi2016@ukr.net


Дніпропетровський національний університет ім. О. Гончара

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