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Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1. / Kazansky, A. Yu; Anoikin, A. A.; Derevianko, A. P. et al.

RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM. ed. / D Nurgaliev; Shcherbakov; A Kosterov; S Spassov. Springer International Publishing AG, 2019. p. 383-409 (Springer Geophysics).

Research output: Chapter in Book/Report/Conference proceedingConference contributionResearchpeer-review

Harvard

Kazansky, AY, Anoikin, AA, Derevianko, AP, Matasova, GG & Bragin, VY 2019, Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1. in D Nurgaliev, Shcherbakov, A Kosterov & S Spassov (eds), RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM. Springer Geophysics, Springer International Publishing AG, pp. 383-409, International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism, Kazan, 01.10.2017. https://doi.org/10.1007/978-3-319-90437-5_27

APA

Kazansky, A. Y., Anoikin, A. A., Derevianko, A. P., Matasova, G. G., & Bragin, V. Y. (2019). Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1. In D. Nurgaliev, Shcherbakov, A. Kosterov, & S. Spassov (Eds.), RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM (pp. 383-409). (Springer Geophysics). Springer International Publishing AG. https://doi.org/10.1007/978-3-319-90437-5_27

Vancouver

Kazansky AY, Anoikin AA, Derevianko AP, Matasova GG, Bragin VY. Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1. In Nurgaliev D, Shcherbakov, Kosterov A, Spassov S, editors, RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM. Springer International Publishing AG. 2019. p. 383-409. (Springer Geophysics). doi: 10.1007/978-3-319-90437-5_27

Author

Kazansky, A. Yu ; Anoikin, A. A. ; Derevianko, A. P. et al. / Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1. RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM. editor / D Nurgaliev ; Shcherbakov ; A Kosterov ; S Spassov. Springer International Publishing AG, 2019. pp. 383-409 (Springer Geophysics).

BibTeX

@inproceedings{5910a9b2da40491bb39f81be8583d656,
title = "Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1",
abstract = "We studied magnetic polarity in four Upper Neogene (Akchagylian stage) sections of Near-Sea Dagestan. Paleomagnetic studies have shown that Shor-Dere section is the most complete section of Late Neogene-Late Quaternary in this territory. The section Rubas-1, which contains Paleolithic artifacts, corresponds to the upper part of the Shor-Dere section, while sections Ajinour and Rubas River are likely short fragments, so their correlation with the reference section is ambiguous. A composite magnetic polarity section of Near-Sea Dagestan was constructed on the base of correlation between Shor-Dere, Rubas-1 and, in part, Rubas River sections. Magnetic polarity pattern of the composite paleomagnetic section is well correlated with the polarity zonation of Akchagylian stage for the neighboring regions of the Caspian basin (Azerbaijan and Turkmenistan), the south of the European part of Russia and the Transcaucasia (the Northern Caspian and the Lower Volga region). Such correlation of the magnetic polarity with those from startotype regions of Akchagylian stage made it possible to identify magnetic polarity zones in the composite section with the magnetic polarity chrons of the Neogene and Quaternary Time Scale (2016). We suggest that the upper part of the composite section can be correlated with Matuyama Chron including Olduvai and Reunion subchrons, while the lower part attributes to Gauss Chron with Kaena subchron. The proposed correlation provides the basis for approximate age estimates for the studied strata and supposes the age of the stone industry from Rubas-1 site not later earlier than 2 million years ago.",
keywords = "Magnetostratigraphy, Near-Sea Dagestan, Akchagylian, Paleolithic",
author = "Kazansky, {A. Yu} and Anoikin, {A. A.} and Derevianko, {A. P.} and Matasova, {G. G.} and Bragin, {V. Yu}",
year = "2019",
doi = "10.1007/978-3-319-90437-5_27",
language = "English",
isbn = "978-3-319-90436-8",
series = "Springer Geophysics",
publisher = "Springer International Publishing AG",
pages = "383--409",
editor = "D Nurgaliev and Shcherbakov and A Kosterov and S Spassov",
booktitle = "RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM",
address = "Switzerland",
note = "International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism ; Conference date: 01-10-2017",

}

RIS

TY - GEN

T1 - Magnetic Polarity Stratigraphy of the Upper Cenozoic Deposits of Near-Sea Dagestan (Russia) and the Age of the Early Paleolithic Site Rubas-1

AU - Kazansky, A. Yu

AU - Anoikin, A. A.

AU - Derevianko, A. P.

AU - Matasova, G. G.

AU - Bragin, V. Yu

PY - 2019

Y1 - 2019

N2 - We studied magnetic polarity in four Upper Neogene (Akchagylian stage) sections of Near-Sea Dagestan. Paleomagnetic studies have shown that Shor-Dere section is the most complete section of Late Neogene-Late Quaternary in this territory. The section Rubas-1, which contains Paleolithic artifacts, corresponds to the upper part of the Shor-Dere section, while sections Ajinour and Rubas River are likely short fragments, so their correlation with the reference section is ambiguous. A composite magnetic polarity section of Near-Sea Dagestan was constructed on the base of correlation between Shor-Dere, Rubas-1 and, in part, Rubas River sections. Magnetic polarity pattern of the composite paleomagnetic section is well correlated with the polarity zonation of Akchagylian stage for the neighboring regions of the Caspian basin (Azerbaijan and Turkmenistan), the south of the European part of Russia and the Transcaucasia (the Northern Caspian and the Lower Volga region). Such correlation of the magnetic polarity with those from startotype regions of Akchagylian stage made it possible to identify magnetic polarity zones in the composite section with the magnetic polarity chrons of the Neogene and Quaternary Time Scale (2016). We suggest that the upper part of the composite section can be correlated with Matuyama Chron including Olduvai and Reunion subchrons, while the lower part attributes to Gauss Chron with Kaena subchron. The proposed correlation provides the basis for approximate age estimates for the studied strata and supposes the age of the stone industry from Rubas-1 site not later earlier than 2 million years ago.

AB - We studied magnetic polarity in four Upper Neogene (Akchagylian stage) sections of Near-Sea Dagestan. Paleomagnetic studies have shown that Shor-Dere section is the most complete section of Late Neogene-Late Quaternary in this territory. The section Rubas-1, which contains Paleolithic artifacts, corresponds to the upper part of the Shor-Dere section, while sections Ajinour and Rubas River are likely short fragments, so their correlation with the reference section is ambiguous. A composite magnetic polarity section of Near-Sea Dagestan was constructed on the base of correlation between Shor-Dere, Rubas-1 and, in part, Rubas River sections. Magnetic polarity pattern of the composite paleomagnetic section is well correlated with the polarity zonation of Akchagylian stage for the neighboring regions of the Caspian basin (Azerbaijan and Turkmenistan), the south of the European part of Russia and the Transcaucasia (the Northern Caspian and the Lower Volga region). Such correlation of the magnetic polarity with those from startotype regions of Akchagylian stage made it possible to identify magnetic polarity zones in the composite section with the magnetic polarity chrons of the Neogene and Quaternary Time Scale (2016). We suggest that the upper part of the composite section can be correlated with Matuyama Chron including Olduvai and Reunion subchrons, while the lower part attributes to Gauss Chron with Kaena subchron. The proposed correlation provides the basis for approximate age estimates for the studied strata and supposes the age of the stone industry from Rubas-1 site not later earlier than 2 million years ago.

KW - Magnetostratigraphy

KW - Near-Sea Dagestan

KW - Akchagylian

KW - Paleolithic

U2 - 10.1007/978-3-319-90437-5_27

DO - 10.1007/978-3-319-90437-5_27

M3 - Conference contribution

SN - 978-3-319-90436-8

T3 - Springer Geophysics

SP - 383

EP - 409

BT - RECENT ADVANCES IN ROCK MAGNETISM, ENVIRONMENTAL MAGNETISM AND PALEOMAGNETISM

A2 - Nurgaliev, D

A2 - Shcherbakov, null

A2 - Kosterov, A

A2 - Spassov, S

PB - Springer International Publishing AG

T2 - International Conference on Geomagnetism, Paleomagnetism and Rock Magnetism

Y2 - 1 October 2017

ER -

ID: 25378159