Publications

Scientific publications

Ю.Е. Дейнес.

Литохимические признаки шунгитоносных горизонтов Онежского синклинория

// Труды КарНЦ РАН. No 11. Сер. Геология Докембрия. 2018. C. 111-115

Yu.E. Deines. Lithochemical features of shungite rocks horizons, Onega structure // Transactions of Karelian Research Centre of Russian Academy of Science. No 11. Precambrian Geology Series. 2018. Pp. 111-115

Keywords: maxovites; petrochemical modules; stratigraphy

The studies of maksovite of Onega structure dome-deposits were carried out. It is developed on different stratigraphic levels of Zaonega Formation of the Palaeoproterozoic (2.0-1.9 Ga). Maksovite were separated for five groups by content of mineral component, namely, supersilites, normosilites, miosilites, gypersilites and siallites. The geochemical features of maksovites are revealed depend on their stratigraphic position and within dome structures.

URL: http://journals.krc.karelia.ru/index.php/precambrian/article/view/846

DOI: 10.17076/geo846

Indexed at RSCI

Last modified: December 3, 2018