Standard

Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region. / Gusev, E.A.; Molodkov, A.N.; Streletskaya, I.D.; Vasiliev, A.A.; Anikina, N.; Bondarenko, S.A.; Derevyanko, L.G.; Kupriyanova, N.V.; Maksimov, F.E.; Polyakova, E.I.; Pushina, Z.V.; Stepanova, G.V.; Oblogov, G.E.

в: Russian Geology and Geophysics, Том 57, № 4, 2016, стр. 586-596.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Gusev, EA, Molodkov, AN, Streletskaya, ID, Vasiliev, AA, Anikina, N, Bondarenko, SA, Derevyanko, LG, Kupriyanova, NV, Maksimov, FE, Polyakova, EI, Pushina, ZV, Stepanova, GV & Oblogov, GE 2016, 'Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region', Russian Geology and Geophysics, Том. 57, № 4, стр. 586-596. https://doi.org/10.1016/j.rgg.2015.05.013

APA

Gusev, E. A., Molodkov, A. N., Streletskaya, I. D., Vasiliev, A. A., Anikina, N., Bondarenko, S. A., Derevyanko, L. G., Kupriyanova, N. V., Maksimov, F. E., Polyakova, E. I., Pushina, Z. V., Stepanova, G. V., & Oblogov, G. E. (2016). Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region. Russian Geology and Geophysics, 57(4), 586-596. https://doi.org/10.1016/j.rgg.2015.05.013

Vancouver

Gusev EA, Molodkov AN, Streletskaya ID, Vasiliev AA, Anikina N, Bondarenko SA и пр. Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region. Russian Geology and Geophysics. 2016;57(4):586-596. https://doi.org/10.1016/j.rgg.2015.05.013

Author

Gusev, E.A. ; Molodkov, A.N. ; Streletskaya, I.D. ; Vasiliev, A.A. ; Anikina, N. ; Bondarenko, S.A. ; Derevyanko, L.G. ; Kupriyanova, N.V. ; Maksimov, F.E. ; Polyakova, E.I. ; Pushina, Z.V. ; Stepanova, G.V. ; Oblogov, G.E. / Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region. в: Russian Geology and Geophysics. 2016 ; Том 57, № 4. стр. 586-596.

BibTeX

@article{445c32c99656473bb83c3bc9bbb51701,
title = "Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region",
abstract = "{\textcopyright} 2015. Dating of marine sediments and faunal remains they contain in stratotype and reference sections by the methods of infrared optically stimulated luminescence (IR-OSL) of K-feldspar, optically stimulated afterglow (OSA) of quartz, electron spin resonance (ESR), and 230Th/U provides new constraints on deposition in the Yenisei mouth during the Kazantsevo interglacial. The luminescence and U-Th ages in the 120-68 ka range and 93-70 ka ESR ages show that the deposition spanned the whole marine isotope stage (MIS) 5. The sediment structures and textures, grain sizes and mineralogy, and faunal records indicate tidal and shelf deposition environments. The sampled assemblages of marine mollusks comprise taxa that typically live in relatively shallow and warm water, as well as abundant subarctic and boreal species, including the Arctica islandica index species. The variations of faunal patterns, more likely, had facies rather than climatic controls, while the sediments were deposited during transgression, in a",
author = "E.A. Gusev and A.N. Molodkov and I.D. Streletskaya and A.A. Vasiliev and N. Anikina and S.A. Bondarenko and L.G. Derevyanko and N.V. Kupriyanova and F.E. Maksimov and E.I. Polyakova and Z.V. Pushina and G.V. Stepanova and G.E. Oblogov",
year = "2016",
doi = "10.1016/j.rgg.2015.05.013",
language = "English",
volume = "57",
pages = "586--596",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier",
number = "4",

}

RIS

TY - JOUR

T1 - Deposits of the Kazantsevo Transgression (MIS 5) in the Northern Yenisei Region

AU - Gusev, E.A.

AU - Molodkov, A.N.

AU - Streletskaya, I.D.

AU - Vasiliev, A.A.

AU - Anikina, N.

AU - Bondarenko, S.A.

AU - Derevyanko, L.G.

AU - Kupriyanova, N.V.

AU - Maksimov, F.E.

AU - Polyakova, E.I.

AU - Pushina, Z.V.

AU - Stepanova, G.V.

AU - Oblogov, G.E.

PY - 2016

Y1 - 2016

N2 - © 2015. Dating of marine sediments and faunal remains they contain in stratotype and reference sections by the methods of infrared optically stimulated luminescence (IR-OSL) of K-feldspar, optically stimulated afterglow (OSA) of quartz, electron spin resonance (ESR), and 230Th/U provides new constraints on deposition in the Yenisei mouth during the Kazantsevo interglacial. The luminescence and U-Th ages in the 120-68 ka range and 93-70 ka ESR ages show that the deposition spanned the whole marine isotope stage (MIS) 5. The sediment structures and textures, grain sizes and mineralogy, and faunal records indicate tidal and shelf deposition environments. The sampled assemblages of marine mollusks comprise taxa that typically live in relatively shallow and warm water, as well as abundant subarctic and boreal species, including the Arctica islandica index species. The variations of faunal patterns, more likely, had facies rather than climatic controls, while the sediments were deposited during transgression, in a

AB - © 2015. Dating of marine sediments and faunal remains they contain in stratotype and reference sections by the methods of infrared optically stimulated luminescence (IR-OSL) of K-feldspar, optically stimulated afterglow (OSA) of quartz, electron spin resonance (ESR), and 230Th/U provides new constraints on deposition in the Yenisei mouth during the Kazantsevo interglacial. The luminescence and U-Th ages in the 120-68 ka range and 93-70 ka ESR ages show that the deposition spanned the whole marine isotope stage (MIS) 5. The sediment structures and textures, grain sizes and mineralogy, and faunal records indicate tidal and shelf deposition environments. The sampled assemblages of marine mollusks comprise taxa that typically live in relatively shallow and warm water, as well as abundant subarctic and boreal species, including the Arctica islandica index species. The variations of faunal patterns, more likely, had facies rather than climatic controls, while the sediments were deposited during transgression, in a

U2 - 10.1016/j.rgg.2015.05.013

DO - 10.1016/j.rgg.2015.05.013

M3 - Article

VL - 57

SP - 586

EP - 596

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 7928438