ПАЛЕОНТОЛОГІЧНІ КРИТЕРІЇ ВИЯВЛЕННЯ СЕДИМЕНТАЦІЙНИХ ПЕРЕРВ У РОЗРІЗІ КАМ’ЯНОВУГІЛЬНИХ ВІДКЛАДІВ ДНІПРОВСЬКО-ДОНЕЦЬКОЇ ЗАПАДИНИ (УКРАЇНА)
DOI:
https://doi.org/10.30836/igs.2522-9753.2023.295190Ключові слова:
стратиграфічний перерив, кам’яновугільна система, Донбас, Дніпровсько-Донецька западинаАнотація
У роботі представлено результати палеонтологічних досліджень мікроскопічних (форамініфери, вапнисті водорості) та макрофауністичних (молюски, кнідарії та інші) решток з кам’яновугільних відкладів Дніпровсько-Донецької западини. За опублікованими, фондовими та власними матеріалами вивчення пошукових свердловин узагальнено та уточнено дані щодо систематичного складу та поширення зазначених груп у міссісіпських і нижньопенсильванських відкладах дослідженого регіону. Розроблено теоретичне підґрунтя палеонтологічних (еволюційних та біостратиграфічних) критеріїв виявлення значущих седиментаційних перерв як потенційних індикаторів нетрадиційних пасток вуглеводнів у розрізі кам’яновугільних відкладів Дніпровсько-Донецької западини.
Посилання
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