Szczegóły publikacji
Opis bibliograficzny
Arctic fold-and-thrust belts / Sergey S. Drachev, Andrey K. Khudoley, Iwona KLONOWSKA, Jarosław MAJKA, Thomas Moore, Karsten Piepjohn, Andrei V. Prokopiev // W: Sedimentary successions of the Arctic region and their hydrocarbon prospectivity [Dokument elektroniczny] / ed. by S. S. Drachev, [et al.]. — Wersja do Windows. — Dane tekstowe. — [London] : Geological Society, 2025. — ( Geological Society Memoir ; ISSN 0435-4052 ; no. 57 ). — S. [1–55]. — Wymagania systemowe: Adobe Reader. — Bibliogr. s. [38–55], Abstr. — Publikacja dostępna online od: 2025-07-28. — I. Klonowska, J. Majka - dod. afiliacja: Uppsala University, Sweden
Autorzy (7)
- Drachev Sergey S.
- Khudoley Andriej
- AGHKlonowska Iwona
- AGHMajka Jarosław
- Moore Thomas
- Piepjohn Karsten
- Prokopiev Andrei V.
Dane bibliometryczne
| ID BaDAP | 161623 |
|---|---|
| Data dodania do BaDAP | 2025-08-29 |
| Tekst źródłowy | URL |
| DOI | 10.1144/M57-2023-30 |
| Rok publikacji | 2025 |
| Typ publikacji | fragment książki |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Memoirs of the Geological Society of London |
Abstract
The modern Arctic has been formed through a series of continent–continent collisions, accretion of terranes and phases of crustal extension. The Neoproterozoic Timanian, Paleozoic Caledonian and Uralian, and late Mesozoic Verkhoyansk–Kolyma, Chukotkan and Brookian orogenies formed several large fold-and-thrust belts (FTBs). The FTBs are exposed across vast areas of continents and continue offshore to form a complex tectonic basement for thick sedimentary basins, playing an important role in the history of accumulation and deformation of younger unmetamorphosed sedimentary successions that are the subject of this volume. Recognition of the importance of FTBs in the Arctic geological history and their role as a controlling factor of development of Arctic sedimentary basins resulted in this chapter, in which we review the current state of knowledge about Arctic FTBs and highlight questions that remain to be addressed. Enclosure D, a map showing boundaries of the FTB and their internal first-order structural fabric, is a part of the overview.
