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Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr. / Shishlov, S. B.; Dubkova, K. A.

In: Lithology and Mineral Resources, Vol. 56, No. 6, 11.2021, p. 509-522.

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

Harvard

Shishlov, SB & Dubkova, KA 2021, 'Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr', Lithology and Mineral Resources, vol. 56, no. 6, pp. 509-522. https://doi.org/10.1134/S0024490221060067

APA

Shishlov, S. B., & Dubkova, K. A. (2021). Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr. Lithology and Mineral Resources, 56(6), 509-522. https://doi.org/10.1134/S0024490221060067

Vancouver

Shishlov SB, Dubkova KA. Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr. Lithology and Mineral Resources. 2021 Nov;56(6):509-522. https://doi.org/10.1134/S0024490221060067

Author

Shishlov, S. B. ; Dubkova, K. A. / Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr. In: Lithology and Mineral Resources. 2021 ; Vol. 56, No. 6. pp. 509-522.

BibTeX

@article{52d6f9c264554ac39d329a7a9abfb2d0,
title = "Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr",
abstract = "Abstract: Upper Paleozoic sections in Taimyr comprise genetic rock complexes of different zones: deep-water shelf; offshore transition zone; shoals, deltas, and beaches of open coasts; bars; shallow lagoons; coastal lagoons; swampy coastal alluvial plain; and drained (distal) alluvial plain. Peculiarities of their spatiotemporal relationships became the basis for compiling paleogeographic schemes of short geological time intervals corresponding to the regional transgressive and regressive maximums. Before the Artinskian (Early Permian), the “Yenisei Land” existed in the southwest, with river systems transporting the terrigenous material to a marine basin opening to the northeast. First signs of the “Kara Land” existence in the north are recorded in the Kungurian sections. In the Middle‒Late Permian, a single “Yenisei–Kara Land” was formed, and the eastern part of Taimyr became a giant lagoon of the “Verkhoyansk Sea.”",
keywords = "depositional environments, genetic rock complexes, paleogeography, Taimyr, terrigenous rocks, Upper Paleozoic",
author = "Shishlov, {S. B.} and Dubkova, {K. A.}",
note = "Publisher Copyright: {\textcopyright} 2021, Pleiades Publishing, Inc.",
year = "2021",
month = nov,
doi = "10.1134/S0024490221060067",
language = "English",
volume = "56",
pages = "509--522",
journal = "Lithology and Mineral Resources",
issn = "0024-4902",
publisher = "МАИК {"}Наука/Интерпериодика{"}",
number = "6",

}

RIS

TY - JOUR

T1 - Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr

AU - Shishlov, S. B.

AU - Dubkova, K. A.

N1 - Publisher Copyright: © 2021, Pleiades Publishing, Inc.

PY - 2021/11

Y1 - 2021/11

N2 - Abstract: Upper Paleozoic sections in Taimyr comprise genetic rock complexes of different zones: deep-water shelf; offshore transition zone; shoals, deltas, and beaches of open coasts; bars; shallow lagoons; coastal lagoons; swampy coastal alluvial plain; and drained (distal) alluvial plain. Peculiarities of their spatiotemporal relationships became the basis for compiling paleogeographic schemes of short geological time intervals corresponding to the regional transgressive and regressive maximums. Before the Artinskian (Early Permian), the “Yenisei Land” existed in the southwest, with river systems transporting the terrigenous material to a marine basin opening to the northeast. First signs of the “Kara Land” existence in the north are recorded in the Kungurian sections. In the Middle‒Late Permian, a single “Yenisei–Kara Land” was formed, and the eastern part of Taimyr became a giant lagoon of the “Verkhoyansk Sea.”

AB - Abstract: Upper Paleozoic sections in Taimyr comprise genetic rock complexes of different zones: deep-water shelf; offshore transition zone; shoals, deltas, and beaches of open coasts; bars; shallow lagoons; coastal lagoons; swampy coastal alluvial plain; and drained (distal) alluvial plain. Peculiarities of their spatiotemporal relationships became the basis for compiling paleogeographic schemes of short geological time intervals corresponding to the regional transgressive and regressive maximums. Before the Artinskian (Early Permian), the “Yenisei Land” existed in the southwest, with river systems transporting the terrigenous material to a marine basin opening to the northeast. First signs of the “Kara Land” existence in the north are recorded in the Kungurian sections. In the Middle‒Late Permian, a single “Yenisei–Kara Land” was formed, and the eastern part of Taimyr became a giant lagoon of the “Verkhoyansk Sea.”

KW - depositional environments

KW - genetic rock complexes

KW - paleogeography

KW - Taimyr

KW - terrigenous rocks

KW - Upper Paleozoic

UR - http://www.scopus.com/inward/record.url?scp=85119409632&partnerID=8YFLogxK

U2 - 10.1134/S0024490221060067

DO - 10.1134/S0024490221060067

M3 - Article

AN - SCOPUS:85119409632

VL - 56

SP - 509

EP - 522

JO - Lithology and Mineral Resources

JF - Lithology and Mineral Resources

SN - 0024-4902

IS - 6

ER -

ID: 91105811