Post-Variscan thermal history of the Moravo-Silesian lower Carboniferous Culm Basin (NE Czech Republic - SW Poland)

• Published in: Tectonophysics 2017-08, Vol.712-713, p.643-662
• Main Authors: Botor, Dariusz, Dunkl, István, Anczkiewicz, Aneta, Mazur, Stanisław
• Format: Article
• Language: English
• Subjects: Age; Apatite; Carboniferous; Cooling; Cretaceous; Ecological succession; Eocene; Fission; Geology; Greywacke; Heat flow; Heat transmission; Heating; Helium; History; Jurassic; Length; Mathematical models; Mesozoic; Modelling; Moravo-Silesian Culm Basin; Mountains; Palaeocene; Paleocene; Paleogene; Permian; Rheno-Hercynian Zone; Standard deviation; Studies; Tectonics; Thermal analysis; Thermal models; Thermochronology; Triassic; Variscides; Zircon
• ISSN: 0040-1951; 1879-3266
• DOI: 10.1016/j.tecto.2017.06.035

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 Nízký Jeseník Mountains. The range of apparent zircon helium ages is 303–233Ma (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 163Ma (Early-Middle Jurassic). Apatite fission track central ages range from 152 (Latest Jurassic) to 44Ma (Eocene), with the majority being grouped between 114 (Aptian) and 57Ma (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 15.4μm. The unimodal track length distribution, the relatively short mean track length (in most samples), and their rather low standard deviation values (1.2 to 2.1μm) 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. •Low-temperature thermochronology was performed in the Moravo-Silesian Culm Basin.•Zircon helium ages range from the late Carboniferous to Middle Jurassic.•Apatite fission track central ages range from the latest Jurassic to Eocene.•Variscan burial caused reaching maximum temperature in the late Carboniferous.•Post-Variscan extension was responsible for re-heating in the Permian-Triassic.