Zobrazeno 1 - 10
of 48
pro vyhledávání: '"K. A. Savko"'
Publikováno v:
Doklady Earth Sciences. 507:1071-1079
Publikováno v:
Geochemistry International. 60:711-723
Publikováno v:
Russian Geology and Geophysics. 62:1175-1187
—The paper presents results of a petrogeochemical and isotope–geochronological study of the granite–leucogranite association of the Pavlov massif and felsic volcanics from the Elash graben (Biryusa block, southwest of the Siberian craton). A ch
Publikováno v:
Geological Journal. 56:4479-4498
Autor:
K. A. Savko, E. H. Korish, V. V. Panevin, A. V. Samsonov, S. V. Tsybulyaev, N. S. Bazikov, R. A. Terentiev
Publikováno v:
Doklady Earth Sciences. 498:412-417
Neoarchean intraplate granitoid (2.61 Ga) and carbonatite magmatism are established in the Kursk block of Sarmatia in close spatial association. Alkaline pyroxenites, carbonatites, and syenites of the Dubravinskii complex are represented by two relat
Publikováno v:
Doklady Earth Sciences. 497:286-290
The age of carbonate rocks of the Tim Formation of the Oskol Group of the Kursk block, Sarmatia, is limited to 2.22–2.10 Ga on the basis of new data on δ13C and 87Sr/86Sr. Carbonate rocks with an anomalously high value of δ13С (about +11‰ V-PD
Publikováno v:
Petrology. 29:114-147
The metabasites of the Tim Formation occur in the Paleoproterozoic Orel, Tim–Yastrebovka, and Avilsky synforms in the Archean Kursk block of Eastern Sarmatia. The volcanics are picrites, picrobasalts, basalts, and basaltic andesites metamorphosed t
Publikováno v:
Geochemistry International. 59:206-211
The paper presents isotope–geochronological data on zircons from a granite–aplite dike that cuts garnet–hypersthene gneisses of the Kuzeyev unit of the Neoarchean–Paleoproterozoic Kan Group in the southern extension of the Ishimba–Tatarka r
Publikováno v:
Doklady Earth Sciences. 495:831-834
The volcanic–terrigenous Tim Formation in the Kursk Block of Sarmatia occurs in the Paleoproterozoic synforms. The Tim Formation volcanics are represented by metamorphosed ferropicrites, ferropicritic basalts, basalts, and andesibasalts. According
Publikováno v:
Russian Geology and Geophysics. 60:1101-1118
—The results of this study reveal the chemical heterogeneity of the Yenisei metamorphic complex, which is a series of blocks within the Yenisei Fault of the southern Yenisei Ridge (Angara–Kan block). The Yenisei complex is composed of four metamo