Recognition of the Cambrian Timan–Severnaya Zemlya orogen and timing of geological evolution of the North Kara sedimentary basin based on detrital zircon dating

• Published in: Doklady earth sciences Vol. 473; no. 2; pp. 402 - 405
• Main Authors: Nikishin, V. A., Malyshev, N. A., Nikishin, A. M., Golovanov, D. Yu, Proskurnin, V. F., Soloviev, A. V., Kulemin, R. F., Morgunova, E. S., Ulyanov, G. V., Fokin, P. A.
• Format: Journal Article
• Language: English
• Published: Moscow Pleiades Publishing 01-04-2017; Springer; Springer Nature B.V
• Subjects: Archipelagoes; Basement rock; Basins; Basins (Geology); Cambrian; Carboniferous; Compression; Deformation; Devonian; Earth and Environmental Science; Earth Sciences; Erosion; Evolution; Geological time; Geology; Granite; Ordovician; Permian; Rock; Rocks; Sandstone; Sedimentary basins; Sediments; Sediments (Geology); Silurian; Weathering; Zircon; Zirconium
• ISSN: 1028-334X; 1531-8354
• DOI: 10.1134/S1028334X17040146

New data on the ages of detrital zircons from folded basement rocks and cover sediments of the Severnaya Zemlya archipelago and Izvestiy TSIK islands have been obtained. The basement age is defined as Cambrian (pre-Ordovician). The Ordovician and Silurian sandstones were mainly formed by erosion of the basement rocks. The Devonian sandstones were formed by debris sourced from the Caledonian orogen. The Carboniferous–Early Permian molasse was formed simultaneously with the erosion of the Carboniferous granitoids and weathering of the Ordovician volcanic arc rocks and the Cambrian basement. The North Kara basin was formed in the Ordovician as a back-arc basin. It experienced its main compression deformations at the boundary of the Devonian and Carboniferous and in the Carboniferous.