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A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley. / Maksimov, F.E.; Zaretskaya, N.E.; Shebotinov, V.V.; Kuznetsov, V.Y.; Uspenskaya, O.N.; Grigoryev, V.A.; Kuksa, K.A.

In: Doklady Earth Sciences, Vol. 462, No. 2, 2015, p. 570-574.

Research output: Contribution to journal › Article › peer-review

Harvard

Maksimov, FE, Zaretskaya, NE, Shebotinov, VV, Kuznetsov, VY, Uspenskaya, ON, Grigoryev, VA & Kuksa, KA 2015, 'A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley', Doklady Earth Sciences, vol. 462, no. 2, pp. 570-574. https://doi.org/10.1134/S1028334X15060185

APA

Maksimov, F. E., Zaretskaya, N. E., Shebotinov, V. V., Kuznetsov, V. Y., Uspenskaya, O. N., Grigoryev, V. A., & Kuksa, K. A. (2015). A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley. Doklady Earth Sciences, 462(2), 570-574. https://doi.org/10.1134/S1028334X15060185

Vancouver

Maksimov FE, Zaretskaya NE, Shebotinov VV, Kuznetsov VY, Uspenskaya ON, Grigoryev VA et al. A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley. Doklady Earth Sciences. 2015;462(2):570-574. https://doi.org/10.1134/S1028334X15060185

Author

Maksimov, F.E. ; Zaretskaya, N.E. ; Shebotinov, V.V. ; Kuznetsov, V.Y. ; Uspenskaya, O.N. ; Grigoryev, V.A. ; Kuksa, K.A. / A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley. In: Doklady Earth Sciences. 2015 ; Vol. 462, No. 2. pp. 570-574.

BibTeX

@article{37bf783aa51d4016bb785e2a1ff786ef,
title = "A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley",
abstract = "The 230Th/U dating results, despite wider confidence intervals relative to the 14C data, may be considered as quite reliable age estimations, which vindicate application of the newer version of isochron approximation for deposits with a low content of organic matter, including buried soils. This establishes a basement for widening capabilities of the 230Th/U method in the field of determination of ages of various lithogenetic types of the Quaternary organogenic sediments, especially those that are older than the limitation of 14C dating.",
author = "F.E. Maksimov and N.E. Zaretskaya and V.V. Shebotinov and V.Y. Kuznetsov and O.N. Uspenskaya and V.A. Grigoryev and K.A. Kuksa",
year = "2015",
doi = "10.1134/S1028334X15060185",
language = "English",
volume = "462",
pages = "570--574",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - A new approach to isotope dating of buried organic-rich deposits with an example from the Kuryador section, upper Vychegda valley

AU - Maksimov, F.E.

AU - Zaretskaya, N.E.

AU - Shebotinov, V.V.

AU - Kuznetsov, V.Y.

AU - Uspenskaya, O.N.

AU - Grigoryev, V.A.

AU - Kuksa, K.A.

PY - 2015

Y1 - 2015

N2 - The 230Th/U dating results, despite wider confidence intervals relative to the 14C data, may be considered as quite reliable age estimations, which vindicate application of the newer version of isochron approximation for deposits with a low content of organic matter, including buried soils. This establishes a basement for widening capabilities of the 230Th/U method in the field of determination of ages of various lithogenetic types of the Quaternary organogenic sediments, especially those that are older than the limitation of 14C dating.

AB - The 230Th/U dating results, despite wider confidence intervals relative to the 14C data, may be considered as quite reliable age estimations, which vindicate application of the newer version of isochron approximation for deposits with a low content of organic matter, including buried soils. This establishes a basement for widening capabilities of the 230Th/U method in the field of determination of ages of various lithogenetic types of the Quaternary organogenic sediments, especially those that are older than the limitation of 14C dating.

U2 - 10.1134/S1028334X15060185

DO - 10.1134/S1028334X15060185

M3 - Article

VL - 462

SP - 570

EP - 574

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 3990676