Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Depositional Environments and Paleogeographic Evolution during the Formation of Upper Paleozoic Terrigenous Rocks in Taimyr. / Shishlov, S. B.; Dubkova, K. A.
в: Lithology and Mineral Resources, Том 56, № 6, 11.2021, стр. 509-522.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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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