Zobrazeno 1 - 10
of 24
pro vyhledávání: '"S. B. Felitsyn"'
Publikováno v:
Paleontological Journal. 55:447-454
The discovery of numerous bacterial remains (including those morphologically similar to modern ironbacteria) in the lower Proterozoic red-colored quartzites of Shoksha, Karelia, and Bolshoy Tyuters Island of the Gulf of Finland, indicates a significa
Autor:
N. A. Alfimova, S. B. Felitsyn
Publikováno v:
Paleontological Journal. 53:757-765
The Fe/Co ratio (ppm) in the kerogen from different-aged clastic sediments (Early Proterozoic–Mesozoic) varies from 17 to 4100, and δ13C value varies from –14.8 to –32.6‰. The relationship between Fe/Co and δ13C is determined by the composi
Autor:
Pritam Nasipuri, Vjacheslav A. Matrenichev, V. Kumar, Mohd Baqar Raza, N. A. Alfimova, Jayanta Kumar Pati, E. S. Bogomolov, S. B. Felitsyn, L. Saha
Publikováno v:
Precambrian Research. 328:1-8
In this communication, we report geochemical and Sm-Nd isotope data of Banded Iron Formation (BIF) from Kola-Karelia (Fennoscandian shield), East-European Platform and Bundelkhand craton, N-E India. The BIFs from Kola-Karelia (Algoma type), and Bunde
Publikováno v:
Paleontological Journal. 51:430-440
Probable microfossils, presumably of bacterial origin, were found in the banded iron formations of Karelia and the Kola Peninsula. The age of these formations is 2.7–2.8 Ga. Based on the organic carbon content and balance estimations it was establi
Autor:
E. S. Bogomolov, S. B. Felitsyn
Publikováno v:
Lithology and Mineral Resources. 51:107-116
Spectra of the REE distribution in the Quaternary–Recent peat bog ore of southern Karelia and Leningrad region are characterized by LaN/YbN < 1.0, presence of positive Eu and negative Ce anomalies, and higher Y enrichment (relative to Ho and Dy) be
Isotope composition of neodymium in neo-Archean banded iron formations of Karelia and Kola Peninsula
Publikováno v:
Doklady Earth Sciences. 465:1268-1271
Studies of three deposits of neo-Archean banded iron formations from the West Karelian domain (the Kostomuksha deposit) and from the Central Kola block (the Olenegorsk and Kirovogorsk deposits) showed a pronounced difference in the isotope compositio
Autor:
T. N. German, S. B. Felitsyn
Publikováno v:
Paleontological Journal. 49:221-229
Study of carbon isotopic composition of micro- and macrofossils and dissipated sedimentary matter (kerogens) extracted by acid maceration from the clay shales from three Riphean, Vendian, and Cambrian sections of the Siberian and East European platfo
Publikováno v:
Doklady Biological Sciences. 470:231-233
Fossilized cyanobacteria(?) represented by trichomes enclosed in common sheaths were detected in early Proterozoic iron banded formations of the Kursk magnetic anomaly (limonite-martite ores of the Lebedinsky mine and iron banded formations of the Ko
Autor:
S. B. Felitsyn, N. A. Alfimova
Publikováno v:
Doklady biological sciences : proceedings of the Academy of Sciences of the USSR, Biological sciences sections. 474(1)
Microelement composition of Gallionella sp.-containing bacterial mats from the environs of St. Petersburg and isotope composition of organic carbon, strontium, and neodymium from these mats have been determined. Isotope and microelement systematics o
Publikováno v:
Lithology and Mineral Resources. 46:397-408
The absence of Ce anomaly and significant positive correlation between Ce and Fe in the weathering profiles and sedimentary carbonate rocks of the Baltic Shield with an age of 2.8–2.1 Ga indicate that Fe3+ was the main form of Fe migration in the A