The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments

N. V. Sennikov; O. T. Obut; T. Yu Tolmacheva; E. V. Lykova; R. A. Khabibulina

doi:10.1016/j.rgg.2018.01.005

The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments

N. V. Sennikov, O. T. Obut, T. Yu Tolmacheva, E. V. Lykova, R. A. Khabibulina

Результат исследования: Научные публикации в периодических изданиях › статья

Аннотация

Comprehensive lithofacies and biofacies analysis provided constraints on the origin of Upper Ordovician clastic and carbonate deposits in northeastern Gorny Altai, which form large low-elevated flat carbonate banks located relatively close to the shore. The sediments were deposited during the Sandbian and early-middle Katian stages, according to new conodont data. Upper Ordovician sections in northeastern Gorny Altai store record of two global regressions: the early Sandbian (Vollen Lowstand) and early Katian (Frognerkilen Lowstand) events.

Язык оригинала	английский
Страницы (с-по)	72-87
Число страниц	16
Журнал	Russian Geology and Geophysics
Том	59
Номер выпуска	1
DOI	https://doi.org/10.1016/j.rgg.2018.01.005
Состояние	Опубликовано - 1 янв 2018

Доступ к документу

10.1016/j.rgg.2018.01.005

Link to publication in Scopus

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Цитировать

Sennikov, N. V., Obut, O. T., Tolmacheva, T. Y., Lykova, E. V., & Khabibulina, R. A. (2018). The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments. Russian Geology and Geophysics, 59(1), 72-87. https://doi.org/10.1016/j.rgg.2018.01.005

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title = "The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments",

abstract = "Comprehensive lithofacies and biofacies analysis provided constraints on the origin of Upper Ordovician clastic and carbonate deposits in northeastern Gorny Altai, which form large low-elevated flat carbonate banks located relatively close to the shore. The sediments were deposited during the Sandbian and early-middle Katian stages, according to new conodont data. Upper Ordovician sections in northeastern Gorny Altai store record of two global regressions: the early Sandbian (Vollen Lowstand) and early Katian (Frognerkilen Lowstand) events.",

keywords = "conodonts, deposition environment, facies, Gorny Altai, Ordovician",

author = "Sennikov, {N. V.} and Obut, {O. T.} and Tolmacheva, {T. Yu} and Lykova, {E. V.} and Khabibulina, {R. A.}",

year = "2018",

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The Upper Ordovician of northeastern Gorny Altai : Stratigraphy and deposition environments. / Sennikov, N. V.; Obut, O. T.; Tolmacheva, T. Yu; Lykova, E. V.; Khabibulina, R. A.

В: Russian Geology and Geophysics, Том 59, № 1, 01.01.2018, стр. 72-87.

Результат исследования: Научные публикации в периодических изданиях › статья

TY - JOUR

T1 - The Upper Ordovician of northeastern Gorny Altai

T2 - Stratigraphy and deposition environments

AU - Sennikov, N. V.

AU - Obut, O. T.

AU - Tolmacheva, T. Yu

AU - Lykova, E. V.

AU - Khabibulina, R. A.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - Comprehensive lithofacies and biofacies analysis provided constraints on the origin of Upper Ordovician clastic and carbonate deposits in northeastern Gorny Altai, which form large low-elevated flat carbonate banks located relatively close to the shore. The sediments were deposited during the Sandbian and early-middle Katian stages, according to new conodont data. Upper Ordovician sections in northeastern Gorny Altai store record of two global regressions: the early Sandbian (Vollen Lowstand) and early Katian (Frognerkilen Lowstand) events.

AB - Comprehensive lithofacies and biofacies analysis provided constraints on the origin of Upper Ordovician clastic and carbonate deposits in northeastern Gorny Altai, which form large low-elevated flat carbonate banks located relatively close to the shore. The sediments were deposited during the Sandbian and early-middle Katian stages, according to new conodont data. Upper Ordovician sections in northeastern Gorny Altai store record of two global regressions: the early Sandbian (Vollen Lowstand) and early Katian (Frognerkilen Lowstand) events.

KW - conodonts

KW - deposition environment

KW - facies

KW - Gorny Altai

KW - Ordovician

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