Szczegóły publikacji
Opis bibliograficzny
Post-Variscan thermal history of the Moravo-Silesian lower Carboniferous Culm Basin (NE Czech Republic - SW Poland) / Dariusz BOTOR, István Dunkl, Aneta Anczkiewicz, Stanisław Mazur // Tectonophysics ; ISSN 0040-1951. — 2017 — vol. 712–713, s. 643–662. — Bibliogr. s. 660–662, Abstr. — Publikacja dostępna online od: 2017-06-30
Autorzy (4)
- AGHBotor Dariusz
- Dunkl István
- Anczkiewicz Aneta A.
- Mazur Stanisław
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 109694 |
|---|---|
| Data dodania do BaDAP | 2017-10-19 |
| Tekst źródłowy | URL |
| DOI | 10.1016/j.tecto.2017.06.035 |
| Rok publikacji | 2017 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Czasopismo/seria | Tectonophysics |
Abstract
Apatite fission track analysis (AFT) and zircon (U-Th)/He thermochronology (ZHe) have been carried out for a lower Carboniferous greywacke succession of the Moravo-Silesian Culm Basin in the Nizky jesera Mountains. The range of apparent zircon helium ages is 303-233 Ma (late Carboniferous to Early Triassic) in the eastern part of the basin, whilst they are significantly younger in the western part, ranging from 194 to 163 Ma (Early Middle Jurassic). Apatite fission track central ages range from 152 (Latest Jurassic) to 44 Ma (Eocene), with the majority being grouped between 114 (Aptian) and 57 Ma (Paleocene). All samples experienced substantial post-depositional thermal reset; both the AFT ages and the ZHe are considerably younger than the depositional ages. The mean track length varies in the range between 12.5 and 15.4 mu m. The unimodal track length distribution, the relatively short mean track length (in most samples), and their rather low standard deviation values (1.2 to 2.1 mu m) indicate that their thermal history was determined by Variscan and post-Variscan heating event(s) followed by a prolonged residence in the apatite partial annealing zone in the Mesozoic and finally by cooling in the Paleogene. Geological evidence combined with thermal modeling based on AFT and ZHe data indicate that the lower Carboniferous strata had already reached maximum palaeotemperatures in the late Carboniferous, however, they were presumably later re-heated during the Permian-Triassic. Post-Variscan extensional tectonics events were responsible for high heat flow that together with Carboniferous burial could account for the reset of both thermochronometers. A major phase of cooling occurred in the Late Cretaceous. Finally, exhumation was probably faster in the Paleogene, causing the present-day exposure of the studied rocks.
