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Silurian terrigenous-carbonate sedimentaion in Gorny Altai : Structure, facies variability, faunal assemblages, and stratigraphic position. / Sennikov, N. V.; Khabibulina, R. A.; Obut, O. T. et al.

In: Russian Geology and Geophysics, Vol. 60, No. 4, 04.2019, p. 451-471.

Research output: Contribution to journal › Article › peer-review

Harvard

Sennikov, NV, Khabibulina, RA, Obut, OT, Novozhilova, NV, Tokarev, DA & Luchinina, VA 2019, 'Silurian terrigenous-carbonate sedimentaion in Gorny Altai: Structure, facies variability, faunal assemblages, and stratigraphic position', Russian Geology and Geophysics, vol. 60, no. 4, pp. 451-471. https://doi.org/10.15372/RGG2019031

APA

Sennikov, N. V., Khabibulina, R. A., Obut, O. T., Novozhilova, N. V., Tokarev, D. A., & Luchinina, V. A. (2019). Silurian terrigenous-carbonate sedimentaion in Gorny Altai: Structure, facies variability, faunal assemblages, and stratigraphic position. Russian Geology and Geophysics, 60(4), 451-471. https://doi.org/10.15372/RGG2019031

Vancouver

Sennikov NV, Khabibulina RA, Obut OT, Novozhilova NV, Tokarev DA, Luchinina VA. Silurian terrigenous-carbonate sedimentaion in Gorny Altai: Structure, facies variability, faunal assemblages, and stratigraphic position. Russian Geology and Geophysics. 2019 Apr;60(4):451-471. doi: 10.15372/RGG2019031

Author

Sennikov, N. V. ; Khabibulina, R. A. ; Obut, O. T. et al. / Silurian terrigenous-carbonate sedimentaion in Gorny Altai : Structure, facies variability, faunal assemblages, and stratigraphic position. In: Russian Geology and Geophysics. 2019 ; Vol. 60, No. 4. pp. 451-471.

BibTeX

@article{3519f7b446ce4b2196fdecce84707f9c,
title = "Silurian terrigenous-carbonate sedimentaion in Gorny Altai: Structure, facies variability, faunal assemblages, and stratigraphic position",
abstract = "This paper discusses the structure and facies variability of the Silurian mixed terrigenous-carbonate strata and presents new paleontological and biostratigraphic data. It attempts to refine the stratigraphic position and provide new lithologic evidence (markers) for regional manifestations of global sedimentary events (Mulde transgressive-regressive and Linde regressive events) in the Altai sections. The chronostratigraphic position of the Kuimov Horizon, a regional stratigraphic unit, has been defined based on graptolite and conodont faunas.",
keywords = "Event stratigraphy, Gorny Altai, Gorstian, Homerian, Ludfordian, Silurian, event stratigraphy",
author = "Sennikov, {N. V.} and Khabibulina, {R. A.} and Obut, {O. T.} and Novozhilova, {N. V.} and Tokarev, {D. A.} and Luchinina, {V. A.}",
year = "2019",
month = apr,
doi = "10.15372/RGG2019031",
language = "English",
volume = "60",
pages = "451--471",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "4",

}

RIS

TY - JOUR

T1 - Silurian terrigenous-carbonate sedimentaion in Gorny Altai

T2 - Structure, facies variability, faunal assemblages, and stratigraphic position

AU - Sennikov, N. V.

AU - Khabibulina, R. A.

AU - Obut, O. T.

AU - Novozhilova, N. V.

AU - Tokarev, D. A.

AU - Luchinina, V. A.

PY - 2019/4

Y1 - 2019/4

N2 - This paper discusses the structure and facies variability of the Silurian mixed terrigenous-carbonate strata and presents new paleontological and biostratigraphic data. It attempts to refine the stratigraphic position and provide new lithologic evidence (markers) for regional manifestations of global sedimentary events (Mulde transgressive-regressive and Linde regressive events) in the Altai sections. The chronostratigraphic position of the Kuimov Horizon, a regional stratigraphic unit, has been defined based on graptolite and conodont faunas.

AB - This paper discusses the structure and facies variability of the Silurian mixed terrigenous-carbonate strata and presents new paleontological and biostratigraphic data. It attempts to refine the stratigraphic position and provide new lithologic evidence (markers) for regional manifestations of global sedimentary events (Mulde transgressive-regressive and Linde regressive events) in the Altai sections. The chronostratigraphic position of the Kuimov Horizon, a regional stratigraphic unit, has been defined based on graptolite and conodont faunas.

KW - Event stratigraphy

KW - Gorny Altai

KW - Gorstian

KW - Homerian

KW - Ludfordian

KW - Silurian

KW - event stratigraphy

UR - http://www.scopus.com/inward/record.url?scp=85064965501&partnerID=8YFLogxK

U2 - 10.15372/RGG2019031

DO - 10.15372/RGG2019031

M3 - Article

AN - SCOPUS:85064965501

VL - 60

SP - 451

EP - 471

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 20042162