Санкт-Петербургский горный университет императрицы Екатерины II, Санкт-Петербург, Россия

Песков Д. В., аспирант
Прищепа О. М., зав. кафедрой, проф., д-р геол.-минерал. наук, prischepa_om@pers.spmi.ru
Жарков А. М., проф., д-р геол.-минерал. наук

Исследовано строение осадочного чехла Мезенско-Бело морско го региона. Основной отличительной чертой Мезенской синеклизы является трехслойное строение осадочного чехла, сложенного породами верхнего протерозоя, венда-кембрия и палеозоя. При небольшой мощности вендско-кембрийской и палеозойской частей осадочного чехла, перспективы нефтегазоносности которых оцениваются крайне низко, мощность средневерхнерифейских отложений составляет на суше 3–5 км, а в акватории достигает 6 км и более, что позволяет оценивать их как самостоятельное направление исследований. Обработка результатов бурения скважины Средне-Няфтинская 21 позволила получить более системное представление о строении древних толщ рифейского возраста.

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