U-Pb zircon age of the Krásné Loučky tuffite: the dating of Visean flysch in the Moravo-Silesian Paleozoic Basin (Rhenohercynian Zone, Czech Republic)

Jirásek, Jakub; Wlosok, Jiří; Martin, Silvana; Matýsek, Dalibor; Schmitz, Mark D.; Sýkorová, Ivana; Vašíček, Zdeněk

doi:10.7306/gq.1201

Cited by 6 publications

(2 citation statements)

References 29 publications

Supporting

Mentioning

Contrasting

Order By: Relevance

“…2). The recently established age of zircons from the tuffite horizon in Krásné Louèky (340.05 ± 0.22 Ma by TIMS U-Pb) corresponds to the Viséan stage and dates the boundary between the Horní Benešov and Moravice formations (Jirásek et al, 2014).…”

Section: Geological Settingmentioning

confidence: 95%

“…The age of the synorogenic siliciclastics in the Culm Basin (Fig. 2) is early Viséan to the earliest Namurian (Dvoøák, 1973;Kumpera, 1983;Zapletal et al, 1989;Dvoøák, 1994;Kalvoda et al, 2008;Jirásek et al, 2014). Lower Carboniferous sediments of the Nízký Jeseník Sub-basin are subdivided into four formations: the Andìlská Hora Fm, the Horni Benešov Fm, the Moravice Fm.…”

Section: Geological Settingmentioning

confidence: 99%

See 1 more Smart Citation

Thermal history of the lower Carboniferous Culm Basin in the Nízký Jeseník Mts. (NE Bohemian Massif, Czech Republic and Poland)

Botor

Toboła

Jelonek

2017

ASGP

View full text Add to dashboard Cite

Raman microspectroscopy of organic matter, vitrinite reflectance and fluid inclusion data were used to reconstruct the thermal history in the lower Carboniferous accretionary prism of the Culm Basin in the Nízký Jeseník Mts. (NE Bohemian Massif). The model involves the Variscan (mid-late Carboniferous) burial diagenesis, which was overprinted by a post-Variscan, probably Permian and/or early Mesozoic, thermal pulse(s) in its central and western parts. The latter may have been related to advective heat transport and the circulation of hot fluids. In the siliciclastic rocks of the Culm Basin, the maximum palaeotemperatures varied from~200 ± 30°C in the E (in the Hradec-Kyjovice Formation) to~350 ± 30°C in the NW (in the Andìlská Hora Formation).

show abstract

Section: Geological Settingmentioning

confidence: 95%

Section: Geological Settingmentioning

confidence: 99%