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Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence. / Kanygin, A. V.; Gonta, T. V.; Timokhin, A. V.

в: Russian Geology and Geophysics, Том 61, № 4, 01.04.2020, стр. 359-377.

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

Harvard

Kanygin, AV, Gonta, TV & Timokhin, AV 2020, 'Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence', Russian Geology and Geophysics, Том. 61, № 4, стр. 359-377. https://doi.org/10.15372/RGG2019139

APA

Kanygin, A. V., Gonta, T. V., & Timokhin, A. V. (2020). Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence. Russian Geology and Geophysics, 61(4), 359-377. https://doi.org/10.15372/RGG2019139

Vancouver

Kanygin AV, Gonta TV, Timokhin AV. Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence. Russian Geology and Geophysics. 2020 апр. 1;61(4):359-377. doi: 10.15372/RGG2019139

Author

Kanygin, A. V. ; Gonta, T. V. ; Timokhin, A. V. / Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence. в: Russian Geology and Geophysics. 2020 ; Том 61, № 4. стр. 359-377.

BibTeX

@article{b09632a58a7f40848930b13a25c35a96,
title = "Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence",
abstract = "The comprehensive chorological analyses of benthic and planktonic faunal groups, the reconstruction of paleogeography, and the delineation and correlation of the same-type biofacies and geographic ranges of the fauna suggest that the Paleozoic tectonic blocks of the Verkhoyansk-Chukotka foldbelt (Tas-Khayakhtakh, Selennyakh, Omulevka, Omolon, Okhotsk, and Chukchi inliers) and Kotel'nyi Island originated in the same epicontinental sea basin of the Siberian paleocontinent, being parts of its passive margin located at the place of the recent foldbelt. We provide a rationale for paleontological, sedimentary, and morphometric diagnostic characteristics of rift zones in complex thrust-folded structures. A rift development, with activation phases in the Ordovician and Devonian, is found to have preceded the break-up of the passive margin in the late Paleozoic.",
keywords = "Chorology, Foldbelt, Northeastern Asia, Paleogeography, Paleozoic, Sedimentology, Siberian paleocontinent, Stratigraphy, Tectonics, Terranes",
author = "Kanygin, {A. V.} and Gonta, {T. V.} and Timokhin, {A. V.}",
year = "2020",
month = apr,
day = "1",
doi = "10.15372/RGG2019139",
language = "English",
volume = "61",
pages = "359--377",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "4",

}

RIS

TY - JOUR

T1 - Position of the Siberian platform and adjacent cratonic terranes in the Paleozoic from paleontological and geological evidence

AU - Kanygin, A. V.

AU - Gonta, T. V.

AU - Timokhin, A. V.

PY - 2020/4/1

Y1 - 2020/4/1

N2 - The comprehensive chorological analyses of benthic and planktonic faunal groups, the reconstruction of paleogeography, and the delineation and correlation of the same-type biofacies and geographic ranges of the fauna suggest that the Paleozoic tectonic blocks of the Verkhoyansk-Chukotka foldbelt (Tas-Khayakhtakh, Selennyakh, Omulevka, Omolon, Okhotsk, and Chukchi inliers) and Kotel'nyi Island originated in the same epicontinental sea basin of the Siberian paleocontinent, being parts of its passive margin located at the place of the recent foldbelt. We provide a rationale for paleontological, sedimentary, and morphometric diagnostic characteristics of rift zones in complex thrust-folded structures. A rift development, with activation phases in the Ordovician and Devonian, is found to have preceded the break-up of the passive margin in the late Paleozoic.

AB - The comprehensive chorological analyses of benthic and planktonic faunal groups, the reconstruction of paleogeography, and the delineation and correlation of the same-type biofacies and geographic ranges of the fauna suggest that the Paleozoic tectonic blocks of the Verkhoyansk-Chukotka foldbelt (Tas-Khayakhtakh, Selennyakh, Omulevka, Omolon, Okhotsk, and Chukchi inliers) and Kotel'nyi Island originated in the same epicontinental sea basin of the Siberian paleocontinent, being parts of its passive margin located at the place of the recent foldbelt. We provide a rationale for paleontological, sedimentary, and morphometric diagnostic characteristics of rift zones in complex thrust-folded structures. A rift development, with activation phases in the Ordovician and Devonian, is found to have preceded the break-up of the passive margin in the late Paleozoic.

KW - Chorology

KW - Foldbelt

KW - Northeastern Asia

KW - Paleogeography

KW - Paleozoic

KW - Sedimentology

KW - Siberian paleocontinent

KW - Stratigraphy

KW - Tectonics

KW - Terranes

UR - http://www.scopus.com/inward/record.url?scp=85089075676&partnerID=8YFLogxK

U2 - 10.15372/RGG2019139

DO - 10.15372/RGG2019139

M3 - Article

AN - SCOPUS:85089075676

VL - 61

SP - 359

EP - 377

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 4

ER -

ID: 24986089