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The age of interglacial peat on the Lower Ob'. / Astakhov, V. I.; Arslanov, Kh A.; Maksimov, F. E.; Kuznetsov, V. Yu; Razina, V. V.; Nazarov, D. V.

в: Doklady Earth Sciences, Том 401, № 2, 23.11.2005, стр. 298-302.

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

Harvard

Astakhov, VI, Arslanov, KA, Maksimov, FE, Kuznetsov, VY, Razina, VV & Nazarov, DV 2005, 'The age of interglacial peat on the Lower Ob'', Doklady Earth Sciences, Том. 401, № 2, стр. 298-302.

APA

Astakhov, V. I., Arslanov, K. A., Maksimov, F. E., Kuznetsov, V. Y., Razina, V. V., & Nazarov, D. V. (2005). The age of interglacial peat on the Lower Ob'. Doklady Earth Sciences, 401(2), 298-302.

Vancouver

Astakhov VI, Arslanov KA, Maksimov FE, Kuznetsov VY, Razina VV, Nazarov DV. The age of interglacial peat on the Lower Ob'. Doklady Earth Sciences. 2005 Нояб. 23;401(2):298-302.

Author

Astakhov, V. I. ; Arslanov, Kh A. ; Maksimov, F. E. ; Kuznetsov, V. Yu ; Razina, V. V. ; Nazarov, D. V. / The age of interglacial peat on the Lower Ob'. в: Doklady Earth Sciences. 2005 ; Том 401, № 2. стр. 298-302.

BibTeX

@article{925347aeab1e4a7a9bf219d9961d31e7,
title = "The age of interglacial peat on the Lower Ob'",
abstract = "Analyzed are the absolute dating and palynological analysis results obtained for mineral peat bog in Ob' river valley, which correct stratigraphic scheme of Western Siberia Upper Pleistocene. The conducted Th/U dating positively indicates that the peat was formed during most warm interglacial period, though its palynological characteristic is substantially different from classic diagrams of last European interglacial period.",
author = "Astakhov, {V. I.} and Arslanov, {Kh A.} and Maksimov, {F. E.} and Kuznetsov, {V. Yu} and Razina, {V. V.} and Nazarov, {D. V.}",
year = "2005",
month = nov,
day = "23",
language = "English",
volume = "401",
pages = "298--302",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "2",

}

RIS

TY - JOUR

T1 - The age of interglacial peat on the Lower Ob'

AU - Astakhov, V. I.

AU - Arslanov, Kh A.

AU - Maksimov, F. E.

AU - Kuznetsov, V. Yu

AU - Razina, V. V.

AU - Nazarov, D. V.

PY - 2005/11/23

Y1 - 2005/11/23

N2 - Analyzed are the absolute dating and palynological analysis results obtained for mineral peat bog in Ob' river valley, which correct stratigraphic scheme of Western Siberia Upper Pleistocene. The conducted Th/U dating positively indicates that the peat was formed during most warm interglacial period, though its palynological characteristic is substantially different from classic diagrams of last European interglacial period.

AB - Analyzed are the absolute dating and palynological analysis results obtained for mineral peat bog in Ob' river valley, which correct stratigraphic scheme of Western Siberia Upper Pleistocene. The conducted Th/U dating positively indicates that the peat was formed during most warm interglacial period, though its palynological characteristic is substantially different from classic diagrams of last European interglacial period.

UR - http://www.scopus.com/inward/record.url?scp=20344385508&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:20344385508

VL - 401

SP - 298

EP - 302

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 35957340