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Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna. / Sennikov, N. V.; Tolmacheva, T. Yu; Obut, O. T. et al.

In: Russian Geology and Geophysics, Vol. 56, No. 4, 01.04.2015, p. 594-610.

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

Harvard

Sennikov, NV, Tolmacheva, TY, Obut, OT, Izokh, NG & Lykova, EV 2015, 'Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna', Russian Geology and Geophysics, vol. 56, no. 4, pp. 594-610. https://doi.org/10.1016/j.rgg.2015.03.010

APA

Sennikov, N. V., Tolmacheva, T. Y., Obut, O. T., Izokh, N. G., & Lykova, E. V. (2015). Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna. Russian Geology and Geophysics, 56(4), 594-610. https://doi.org/10.1016/j.rgg.2015.03.010

Vancouver

Sennikov NV, Tolmacheva TY, Obut OT, Izokh NG, Lykova EV. Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna. Russian Geology and Geophysics. 2015 Apr 1;56(4):594-610. doi: 10.1016/j.rgg.2015.03.010

Author

Sennikov, N. V. ; Tolmacheva, T. Yu ; Obut, O. T. et al. / Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna. In: Russian Geology and Geophysics. 2015 ; Vol. 56, No. 4. pp. 594-610.

BibTeX

@article{40a32929c6964ba7800a1ff3641d0d14,
title = "Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna",
abstract = "We summarize data on the biostratigraphic units of the Siberian Ordovician deposits based on pelagic groups of fauna: graptolites, conodonts, and chitinozoans. It is shown that graptolite and conodont zones and beds have a high potential for correlation. We have determined the precise zonal position of most of the lower boundaries of the Ordovician stages and informal Ordovician substages of the International Stratigraphic Chart in the Lower Paleozoic key sections of the Taimyr Peninsula, Siberian Platform, and Altai-Sayan Folded Area.",
keywords = "Conodonts, Graptolites, Ordovician, Siberia, Stratigraphy, Zones",
author = "Sennikov, {N. V.} and Tolmacheva, {T. Yu} and Obut, {O. T.} and Izokh, {N. G.} and Lykova, {E. V.}",
year = "2015",
month = apr,
day = "1",
doi = "10.1016/j.rgg.2015.03.010",
language = "English",
volume = "56",
pages = "594--610",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "4",

}

RIS

TY - JOUR

T1 - Zonation of the Siberian Ordovician deposits based on pelagic groups of fauna

AU - Sennikov, N. V.

AU - Tolmacheva, T. Yu

AU - Obut, O. T.

AU - Izokh, N. G.

AU - Lykova, E. V.

PY - 2015/4/1

Y1 - 2015/4/1

N2 - We summarize data on the biostratigraphic units of the Siberian Ordovician deposits based on pelagic groups of fauna: graptolites, conodonts, and chitinozoans. It is shown that graptolite and conodont zones and beds have a high potential for correlation. We have determined the precise zonal position of most of the lower boundaries of the Ordovician stages and informal Ordovician substages of the International Stratigraphic Chart in the Lower Paleozoic key sections of the Taimyr Peninsula, Siberian Platform, and Altai-Sayan Folded Area.

AB - We summarize data on the biostratigraphic units of the Siberian Ordovician deposits based on pelagic groups of fauna: graptolites, conodonts, and chitinozoans. It is shown that graptolite and conodont zones and beds have a high potential for correlation. We have determined the precise zonal position of most of the lower boundaries of the Ordovician stages and informal Ordovician substages of the International Stratigraphic Chart in the Lower Paleozoic key sections of the Taimyr Peninsula, Siberian Platform, and Altai-Sayan Folded Area.

KW - Conodonts

KW - Graptolites

KW - Ordovician

KW - Siberia

KW - Stratigraphy

KW - Zones

UR - http://www.scopus.com/inward/record.url?scp=84927923704&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.03.010

DO - 10.1016/j.rgg.2015.03.010

M3 - Article

AN - SCOPUS:84927923704

VL - 56

SP - 594

EP - 610

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 25758112