Devonian organic massif in the basins of the rivers Kara-Silovayaha (the southest Pai-Hoi)
Authors:
About authors
- Saint Petersburg State Mining University
Abstract
The results of biostratigraphic and litologo-genetic researches in the basins of the rivers Kara and Silovoyaha in the southest Pai-Hoi have allowed to ascertain existence Devonian organic massif – a huge geological substance which thickness is about 1700 m and occupies the space not less than 400 km2. Features of its structure are revealed and the formation history is reconstructed.
References
- Першина А.И. Новые данные по стратиграфии силурийских и девонских отложений юго-восточного окончания Пай-Хоя / А.И.Першина, В.С.Цыганко // Фанерозой Севера европейской части СССР. Сыктывкар, 1980. С. 3-19.
- Антошкина А.И. Эволюция рифообразования и биогенных каркасов в палеозое северо-востока Европейской платформы // Вестник Института геологии. 2005. № 5. С. 10-13.
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