Open AccessNEW DATA ON AGE AND NATURE OF CARBONIZATION WITHIN SOUTHERN FLANK OF THE BAIKAL LEDGE OF THE SIBERIAN CRATON BASEMENT
Author(s) -
Yu. V. Danilova,
V. B. Savelyeva,
Т. Г. Шумилова,
Alexei V. Ivanov,
Б. С. Данилов,
Е. П. Базарова
Publication year - 2017
Publication title -
geodinamika i tektonofizika
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.336
H-Index - 8
ISSN - 2078-502X
DOI - 10.5800/gt-2017-8-3-0257
Subject(s) - craton , geology , basement , geochemistry , paleontology , arc (geometry) , archaeology , geography , tectonics , geometry , mathematics
The Baikal ledge rock formations in the Siberian craton structure are included in the Akitkan mobile belt which is considered as the Late Paleoproterozoic independent island arc system moved up to the ancient basement during the terrains amalgamation 1.91–2.00 Ga ago (Fig. 1) [Rosen, 2003; Gladkochub et al., 2009; Didenko et al., 2013]