Standard

On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods. / Arslanov, K.A.; Yanina, T.A.; Chepalyga, A.L.; Svitoch, A.A.; Makshaev, R.R.; Maksimov, F.E.; Chernov, S.B.; Tertychniy, N.I.; Starikova, A.A.

в: Quaternary International, Том 409, 2016, стр. 81-87.

Результаты исследований: Научные публикации в периодических изданиях › статья

Harvard

Arslanov, KA, Yanina, TA, Chepalyga, AL, Svitoch, AA, Makshaev, RR, Maksimov, FE, Chernov, SB, Tertychniy, NI & Starikova, AA 2016, 'On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods', Quaternary International, Том. 409, стр. 81-87. https://doi.org/10.1016/j.quaint.2015.05.067

APA

Arslanov, K. A., Yanina, T. A., Chepalyga, A. L., Svitoch, A. A., Makshaev, R. R., Maksimov, F. E., Chernov, S. B., Tertychniy, N. I., & Starikova, A. A. (2016). On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods. Quaternary International, 409, 81-87. https://doi.org/10.1016/j.quaint.2015.05.067

Vancouver

Arslanov KA, Yanina TA, Chepalyga AL, Svitoch AA, Makshaev RR, Maksimov FE и пр. On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods. Quaternary International. 2016;409:81-87. https://doi.org/10.1016/j.quaint.2015.05.067

Author

Arslanov, K.A. ; Yanina, T.A. ; Chepalyga, A.L. ; Svitoch, A.A. ; Makshaev, R.R. ; Maksimov, F.E. ; Chernov, S.B. ; Tertychniy, N.I. ; Starikova, A.A. / On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods. в: Quaternary International. 2016 ; Том 409. стр. 81-87.

BibTeX

@article{b99786d6c2214bf48d131302898aff89,
title = "On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods",
abstract = "{\textcopyright} 2015. During the second half of the late Pleistocene, the Caspian experienced repeated transgressions (Early and Late Khvalynian) and regressions (Enotaevsk and Mangyshlak) with an oscillation amplitude of 120-150m. The question about the age of the Khvalynian deposits is controversial. The investigation presents the age chronology of the Khvalynian deposits of the Caspian coasts on the basis of marine terrace stratigraphy and 14C and 230Th/234U dating conducted in the Laboratory of the Saint-Petersburg State University. Forty samples of mollusc material from Khvalynian deposits were dated. For dating, the shells of index-genus Didacna from the deposits of marine terraces with different elevations were sampled. Besides shells, a fragment of bone from Equus sp. was dated. The analysis of dating showed that during the maximum of the Late Valdai (Wurm) glaciation the Khvalynian basin was in a regressive situation. The maximum stage (+48 to+50m) of the Early Khvalynian transgres",
author = "K.A. Arslanov and T.A. Yanina and A.L. Chepalyga and A.A. Svitoch and R.R. Makshaev and F.E. Maksimov and S.B. Chernov and N.I. Tertychniy and A.A. Starikova",
year = "2016",
doi = "10.1016/j.quaint.2015.05.067",
language = "English",
volume = "409",
pages = "81--87",
journal = "Quaternary International",
issn = "1040-6182",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - On the age of the Khvalynian deposits of the Caspian Sea coasts according to 14C and 230Th/234U methods

AU - Arslanov, K.A.

AU - Yanina, T.A.

AU - Chepalyga, A.L.

AU - Svitoch, A.A.

AU - Makshaev, R.R.

AU - Maksimov, F.E.

AU - Chernov, S.B.

AU - Tertychniy, N.I.

AU - Starikova, A.A.

PY - 2016

Y1 - 2016

N2 - © 2015. During the second half of the late Pleistocene, the Caspian experienced repeated transgressions (Early and Late Khvalynian) and regressions (Enotaevsk and Mangyshlak) with an oscillation amplitude of 120-150m. The question about the age of the Khvalynian deposits is controversial. The investigation presents the age chronology of the Khvalynian deposits of the Caspian coasts on the basis of marine terrace stratigraphy and 14C and 230Th/234U dating conducted in the Laboratory of the Saint-Petersburg State University. Forty samples of mollusc material from Khvalynian deposits were dated. For dating, the shells of index-genus Didacna from the deposits of marine terraces with different elevations were sampled. Besides shells, a fragment of bone from Equus sp. was dated. The analysis of dating showed that during the maximum of the Late Valdai (Wurm) glaciation the Khvalynian basin was in a regressive situation. The maximum stage (+48 to+50m) of the Early Khvalynian transgres

AB - © 2015. During the second half of the late Pleistocene, the Caspian experienced repeated transgressions (Early and Late Khvalynian) and regressions (Enotaevsk and Mangyshlak) with an oscillation amplitude of 120-150m. The question about the age of the Khvalynian deposits is controversial. The investigation presents the age chronology of the Khvalynian deposits of the Caspian coasts on the basis of marine terrace stratigraphy and 14C and 230Th/234U dating conducted in the Laboratory of the Saint-Petersburg State University. Forty samples of mollusc material from Khvalynian deposits were dated. For dating, the shells of index-genus Didacna from the deposits of marine terraces with different elevations were sampled. Besides shells, a fragment of bone from Equus sp. was dated. The analysis of dating showed that during the maximum of the Late Valdai (Wurm) glaciation the Khvalynian basin was in a regressive situation. The maximum stage (+48 to+50m) of the Early Khvalynian transgres

U2 - 10.1016/j.quaint.2015.05.067

DO - 10.1016/j.quaint.2015.05.067

M3 - Article

VL - 409

SP - 81

EP - 87

JO - Quaternary International

JF - Quaternary International

SN - 1040-6182

ER -

ID: 7928468