Lithological Signatures of Early Carboniferous Events in the Northeastern Siberian Craton (Western Verkhoyansk Region)

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Lithological Signatures of Early Carboniferous Events in the Northeastern Siberian Craton (Western Verkhoyansk Region). / Sennikov, N. V.; Khabibulina, R. A.; Obut, O. T. et al.

In: Russian Geology and Geophysics, Vol. 63, No. 4, 04.2022, p. 417-434.

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

BibTeX

@article{90c7b901c8b6480ebca0f09d077b1fa8,

title = "Lithological Signatures of Early Carboniferous Events in the Northeastern Siberian Craton (Western Verkhoyansk Region)",

abstract = "The paper focuses on presumable sources of coarse carbonate material transported into the Visean Northern Kharaulakh basin. The sand to pebble components of the Krestyakh conglomerate unit originated by medium and distant transport by debris flows (turbidity currents) along submarine canyons from the place of their initial littoral deposition to relatively deep accommodation basins. The carbonate material was most likely derived from Ordovician, Silurian, and Devonian sediments, which are currently represented by their analogs in Kotelny Island. The sediments of the Northern Kharaulakh basin store a record of two geological events: (1) middle Visean collision of Siberia with the Laurussian supercontinent and rifting of some terranes off the Siberian сraton, and (2) late Visean collision of the Kara terrane with the northern margin of Siberia.",

keywords = "Carboniferous, conodonts, geological events, lithology, ostracods, paleogeography, redeposited fauna assemblage, tabulate corals, Visean, Western Verkhoyansk region",

author = "Sennikov, {N. V.} and Khabibulina, {R. A.} and Obut, {O. T.} and Gonta, {T. V.}",

note = "Funding Information: The study was carried out within the framework of the State Assignment of the Russian Academy of Sciences (FWZZ20220003) and was supported by grant 1805-70035 from the Russian Foundation for Basic Research. Publisher Copyright: {\textcopyright} 2022, Novosibirsk State University.",

year = "2022",

month = apr,

doi = "10.2113/RGG20214407",

language = "English",

volume = "63",

pages = "417--434",

journal = "Russian Geology and Geophysics",

issn = "1068-7971",

publisher = "Elsevier Science B.V.",

number = "4",

}

RIS

TY - JOUR

T1 - Lithological Signatures of Early Carboniferous Events in the Northeastern Siberian Craton (Western Verkhoyansk Region)

AU - Sennikov, N. V.

AU - Khabibulina, R. A.

AU - Obut, O. T.

AU - Gonta, T. V.

N1 - Funding Information: The study was carried out within the framework of the State Assignment of the Russian Academy of Sciences (FWZZ20220003) and was supported by grant 1805-70035 from the Russian Foundation for Basic Research. Publisher Copyright: © 2022, Novosibirsk State University.

PY - 2022/4

Y1 - 2022/4

N2 - The paper focuses on presumable sources of coarse carbonate material transported into the Visean Northern Kharaulakh basin. The sand to pebble components of the Krestyakh conglomerate unit originated by medium and distant transport by debris flows (turbidity currents) along submarine canyons from the place of their initial littoral deposition to relatively deep accommodation basins. The carbonate material was most likely derived from Ordovician, Silurian, and Devonian sediments, which are currently represented by their analogs in Kotelny Island. The sediments of the Northern Kharaulakh basin store a record of two geological events: (1) middle Visean collision of Siberia with the Laurussian supercontinent and rifting of some terranes off the Siberian сraton, and (2) late Visean collision of the Kara terrane with the northern margin of Siberia.

AB - The paper focuses on presumable sources of coarse carbonate material transported into the Visean Northern Kharaulakh basin. The sand to pebble components of the Krestyakh conglomerate unit originated by medium and distant transport by debris flows (turbidity currents) along submarine canyons from the place of their initial littoral deposition to relatively deep accommodation basins. The carbonate material was most likely derived from Ordovician, Silurian, and Devonian sediments, which are currently represented by their analogs in Kotelny Island. The sediments of the Northern Kharaulakh basin store a record of two geological events: (1) middle Visean collision of Siberia with the Laurussian supercontinent and rifting of some terranes off the Siberian сraton, and (2) late Visean collision of the Kara terrane with the northern margin of Siberia.

KW - Carboniferous

KW - conodonts

KW - geological events

KW - lithology

KW - ostracods

KW - paleogeography

KW - redeposited fauna assemblage

KW - tabulate corals

KW - Visean

KW - Western Verkhoyansk region

UR - http://www.scopus.com/inward/record.url?scp=85140439434&partnerID=8YFLogxK

UR - https://www.mendeley.com/catalogue/9a4a1d0a-3704-37da-a703-3e7246edf816/

U2 - 10.2113/RGG20214407

DO - 10.2113/RGG20214407

M3 - Article

AN - SCOPUS:85140439434

VL - 63

SP - 417

EP - 434

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 38378522