The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data

The Lower Kazanian sedimentary succession was considered based on the data from the lithological and stratigraphic description and ESR obtained for the outcrop section within the basin of the Sheshma and Inesh Rivers (Republic of Tatarstan). The Lower Kazanian facial composition correlates with the...

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Main Authors: E.I. Fakhrutdinov, N.G. Nurgalieva, N.M. Khassanova, V.V. Silantiev
Format: Article
Language:English
Published: Kazan Federal University 2015-09-01
Series:Učënye Zapiski Kazanskogo Universiteta. Seriâ Estestvennye Nauki
Subjects:
Online Access:https://kpfu.ru/portal/docs/F_184141641/157_3_est_8_e.pdf
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author E.I. Fakhrutdinov
N.G. Nurgalieva
N.M. Khassanova
V.V. Silantiev
author_facet E.I. Fakhrutdinov
N.G. Nurgalieva
N.M. Khassanova
V.V. Silantiev
author_sort E.I. Fakhrutdinov
collection DOAJ
description The Lower Kazanian sedimentary succession was considered based on the data from the lithological and stratigraphic description and ESR obtained for the outcrop section within the basin of the Sheshma and Inesh Rivers (Republic of Tatarstan). The Lower Kazanian facial composition correlates with the specific composition and variations of the paramagnetic centers Mn2+, SO3–, SO2–, PO2–, C600, and E'. These ESR labels can be used as facial and chemostratigraphic criteria to stratify and correlate the Lower Kazanian sections in Volga-Kama region.
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spelling doaj.art-76a68f7ea0ae492ca7f70519548c2fa52023-06-07T13:55:24ZengKazan Federal UniversityUčënye Zapiski Kazanskogo Universiteta. Seriâ Estestvennye Nauki2542-064X2500-218X2015-09-01157387101The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR DataE.I. Fakhrutdinov0 N.G. Nurgalieva1N.M. Khassanova2 V.V. Silantiev3Kazan Federal University, Kazan, 420008 RussiaKazan Federal University, Kazan, 420008 RussiaKazan Federal University, Kazan, 420008 RussiaKazan Federal University, Kazan, 420008 RussiaThe Lower Kazanian sedimentary succession was considered based on the data from the lithological and stratigraphic description and ESR obtained for the outcrop section within the basin of the Sheshma and Inesh Rivers (Republic of Tatarstan). The Lower Kazanian facial composition correlates with the specific composition and variations of the paramagnetic centers Mn2+, SO3–, SO2–, PO2–, C600, and E'. These ESR labels can be used as facial and chemostratigraphic criteria to stratify and correlate the Lower Kazanian sections in Volga-Kama region.https://kpfu.ru/portal/docs/F_184141641/157_3_est_8_e.pdflower kazanian substagepaleoenvironmentesr
spellingShingle E.I. Fakhrutdinov
N.G. Nurgalieva
N.M. Khassanova
V.V. Silantiev
The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data
Učënye Zapiski Kazanskogo Universiteta. Seriâ Estestvennye Nauki
lower kazanian substage
paleoenvironment
esr
title The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data
title_full The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data
title_fullStr The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data
title_full_unstemmed The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data
title_short The Lower Kazanian Substage in the Key Section: Lithologies and Paleoenvironments Based on the ESR Data
title_sort lower kazanian substage in the key section lithologies and paleoenvironments based on the esr data
topic lower kazanian substage
paleoenvironment
esr
url https://kpfu.ru/portal/docs/F_184141641/157_3_est_8_e.pdf
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