Standard

The Upper Ordovician of northeastern Gorny Altai : Stratigraphy and deposition environments. / Sennikov, N. V.; Obut, O. T.; Tolmacheva, T. Yu и др.

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

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

Harvard

Sennikov, NV, Obut, OT, Tolmacheva, TY, Lykova, EV & Khabibulina, RA 2018, 'The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments', Russian Geology and Geophysics, Том. 59, № 1, стр. 72-87. https://doi.org/10.1016/j.rgg.2018.01.005

APA

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

Vancouver

Sennikov NV, Obut OT, Tolmacheva TY, Lykova EV, Khabibulina RA. The Upper Ordovician of northeastern Gorny Altai: Stratigraphy and deposition environments. Russian Geology and Geophysics. 2018 янв. 1;59(1):72-87. doi: 10.1016/j.rgg.2018.01.005

Author

Sennikov, N. V. ; Obut, O. T. ; Tolmacheva, T. Yu и др. / The Upper Ordovician of northeastern Gorny Altai : Stratigraphy and deposition environments. в: Russian Geology and Geophysics. 2018 ; Том 59, № 1. стр. 72-87.

BibTeX

@article{86f7072943e84ebd8f6acd3956e03563,
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",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2018.01.005",
language = "English",
volume = "59",
pages = "72--87",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1",

}

RIS

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

UR - http://www.scopus.com/inward/record.url?scp=85044785059&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.01.005

DO - 10.1016/j.rgg.2018.01.005

M3 - Article

AN - SCOPUS:85044785059

VL - 59

SP - 72

EP - 87

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1

ER -

ID: 12300109