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, J.; Wlosok, J.; Sivek, M.; Matýsek, D.; Schmitz, M.; Sýkorová, I.; Vašíèek, Z.

doi:10.7306/gq.1201

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Tytuł artykułu

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

Autorzy

Jirásek J. , Wlosok J. , Sivek M. , Matýsek D. , Schmitz M. , Sýkorová I. , Vašíèek Z.

Treść / Zawartość

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Jirasek_J_U-PB_Geol. Quart._Vol. 58_No 4_2014.pdf

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DOI

10.7306/gq.1201

Warianty tytułu

Języki publikacji

Abstrakty

The only previous U-Pb zircon date for the the Early Carboniferous flysch sequence of the Moravo-Silesian Paleozoic Basin was published in 1987 from tuffogenic material from Kobylí Quarry at Krásné Loučky near the town of Krnov (Silesia, Czech Republic). The measured age of 319 Ma did not agree with its stratigraphic position, and was used as the basis for a hypothesized block of Late Carboniferous paralic molasse incorporated during a later tectonic event. During a survey of the still active quarry in 2010, volcaniclastic horizons were identified and sampled. Direct correspondence of the tuff units to those sampled in 1987 cannot be proved but is likely. High precision chemical abrasion - thermal ionization mass spectrometry (CA-TIMS) U-Pb dating of zircon from this new material has yielded an age of 340.05 ± 0.22 Ma, which correlates to the previously inferred stratigraphic age of the locality and the current calibration of the Early Carboniferous geologic time scale. The newly established age corresponds to the Visean stage and dates the boundary between the Horní Benešov and Moravice formations that can be correlated with other foredeep basins of the Culm in the European Variscides. A population of detrital Cambro-Ordovician zircons and a single 2.0 Ga old zircon crystal from the same volcaniclastic layer dated by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS) are consistent with the known age of source material in the Variscan orogenic front.

Słowa kluczowe

volcaniclastic sediment Horní Benešov Formation Variscan foreland Viséan Carboniferous chronostratigraphy

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2014

Tom

Vol. 58, No. 4

Strony

659–--672

Opis fizyczny

Bibliogr. 71 poz., rys., tab.

Twórcy

autor

Jirásek J.

jakub.jirasek@vsb.cz

VŠB – Technical University of Ostrava, Faculty of Mining and Geology, 17 listopadu 15/2172, 708 33 Ostrava-Poruba, Czech Republic

autor

Wlosok J.

VŠB – Technical University of Ostrava, Faculty of Mining and Geology, 17 listopadu 15/2172, 708 33 Ostrava-Poruba, Czech Republic

autor

Sivek M.

VŠB – Technical University of Ostrava, Faculty of Mining and Geology, 17 listopadu 15/2172, 708 33 Ostrava-Poruba, Czech Republic

autor

Matýsek D.

VŠB – Technical University of Ostrava, Faculty of Mining and Geology, 17 listopadu 15/2172, 708 33 Ostrava-Poruba, Czech Republic

autor

Schmitz M.

Boise State University, Department of Geosciences, 1910 Uni ver sity Drive, Boise, ID, U.S.A

autor

Sýkorová I.

Academy of Sciences of the Czech Republic, Insti tute of Rock Structure and Mechan ics, V Holešovièkách 41, 182 09 Praha 8, Czech Republic

autor

Vašíèek Z.

Academy of Sciences of the Czech Republic, Institute of Geonics, Studentská 1768, 708 00 Ostrava-Poruba, Czech Republic

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