Zobrazeno 1 - 10
of 31
pro vyhledávání: '"G. A. Karlova"'
Publikováno v:
Геодинамика и тектонофизика, Vol 14, Iss 3 (2023)
The Precambrian to Cambrian strata at the southwestern margin of the Siberian Platform are ubiquitously characterized by a gradual transition from red-colored alluvial and deltaic deposits to shallow-marine carbonates, reflecting a transgressive infi
Externí odkaz:
https://doaj.org/article/13f08e7f4b6e4ce0a8b12ba8e51f6339
Autor:
A. V. Shatsillo, S. V. Rud’ko, N. B. Kuznetsov, T. V. Romanyuk, G. A. Karlova, Boris G. Pokrovsky, Alena A. Kolesnikova, Vasiliy V. Marusin, B. B. Kochnev, A.S. Dubenskiy, S. M. Lyapunov, V. S. Sheshukov
Publikováno v:
Geological Magazine. 158:1156-1172
A number of ecological and geochemical transformations occurred during late Ediacaran and early Cambrian time, the effects of which are difficult to overestimate. However, the strong linkage of biostratigraphic and chemostratigraphic methods with lit
Publikováno v:
Lethaia. 52:464-485
Autor:
G. A. Karlova, Vasiliy V. Marusin, B. B. Kochnev, Huan Cui, Alan J. Kaufman, Dmitriy V. Grazhdankin, K.E. Nagovitsin, Sara Peek, Zhiger Sarsembaev, Olga P. Izokh, Georgiy E. Markov
The concept of the Tommotian Regional Stage of the Siberian Platform has been closely linked to the idea of the ‘Cambrian Explosion’ of animals and protists when the entire Earth system shifted rapidly into Phanerozoic mode. We conducted a multid
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2d625a14cd880f4839071b088250d78
https://hdl.handle.net/20.500.14017/a0f28786-c5b7-4a9c-89b9-9248d764ff2f
https://hdl.handle.net/20.500.14017/a0f28786-c5b7-4a9c-89b9-9248d764ff2f
Publikováno v:
Journal of Physics: Conference Series. 2140:012007
The paper investigates the behavior of Hall-effect sensors (HES) operating in microwave frequency range. In order to evaluate the capabilities of small radars based on HES’s, the calculation of HES output voltage dependence on microwave intensity i
Publikováno v:
Estudios Geologicos, Vol 75, Iss 2, Pp e104-e104 (2019)
En Siberia los morfotipos de Cloudina han sido tradicionalmente considerados como una variedad tafonómica de conchas de Anabarites, insertadas una dentro de otra, bajo condiciones hidrodinámicas específicas. Las asociaciones de conchas cónicas te
Publikováno v:
Journal of Physics: Conference Series. 1488:012028
The paper focuses on the investigation of the possibility to use GaAs Hall-effect sensors (detectors) in active magnetic positioning systems. On the basis of the avalanche S-diode a pulsed magnetic field generator with the pulse front width of 0.3 ns
Autor:
G. A. Karlova, K.E. Nagovitsin, Vasiliy V. Marusin, B. B. Kochnev, Dmitriy V. Grazhdankin, V Rogov
Publikováno v:
Russian Geology and Geophysics. 56:573-583
The first biozone (Anabarites trisulcatus Assemblage Zone) in the Siberian hypostratotype of the Vendian (northwestern slope of the Olenek Uplift) is represented by the Turkut Formation of the Khorbusuonka Group and most of the Syhargalakh Formation
Autor:
S.V. Saraev, Dmitriy V. Grazhdankin, K.E. Nagovitsin, G. A. Karlova, V.A. Kontorovich, B. B. Kochnev, A.E. Kontorovich, G.O. Fedyanin, A.S. Efimov, A. A. Terleev, Yu.F. Filippov
Publikováno v:
Russian Geology and Geophysics. 56:560-572
Fossiliferous Upper Vendian strata are discovered in the Upper Proterozoic to Lower Paleozoic Fore-Yenisei sedimentary basin under a thick Mesozoic–Cenozoic cover in southeastern West Siberia. Two depositional systems are recognized based on sedime
Autor:
I.V. Korovnikov, G. A. Karlova, Yu.F. Filippov, A.I. Varlamov, A. A. Postnikov, D. A. Tokarev, V.A. Kontorovich, A. A. Terleev, A.S. Efimov, I.A. Gubin, B. B. Kochnev, A.E. Kontorovich, K.E. Nagovitsin, T.P. Baturina, N.V. Sennikov, V. A. Luchinina, S.V. Saraev, Yu.A. Filiptsov, N.V. Novozhilova
Publikováno v:
Russian Geology and Geophysics. 53:972-981
The study presents a description of a new type of Cambrian section penetrated in Vostok 4 well in the southeastern part of the West Siberian geosyneclise (Krasnoyarsk Territory). The drilled succession is well characterized by the fossil evidence and