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Multiphase cooling and exhumation of the Krkonoše Piedmont Basin during Mesozoic - Cenozoic basin inversion based on apatite fission track analysis
- 1.0313414 - GLÚ 2009 US eng A - Abstract
Martínek, K. - Svojtka, Martin - Filip, Jiří
Multiphase cooling and exhumation of the Krkonoše Piedmont Basin during Mesozoic - Cenozoic basin inversion based on apatite fission track analysis.
[Vícefázové chladnutí a exhumace podkrkonošské pánve během mesozoicko - kenozoické pánevní inverze na základě apatitové fission track metody.]
ICP Information Newsletter. Roč. 34, 4/6 (2008), s. 1353003-1353003. ISSN 0161-6951.
[International Geological Congress /33./. 06.08.2008-14.08.2008, Oslo]
R&D Projects: GA AV ČR KJB3111305
Institutional research plan: CEZ:AV0Z30130516
Keywords : fission track * apatite * Krkonoše Piedmont basin
Subject RIV: DB - Geology ; Mineralogy
The regional thermal history of the KPB, has been assessed using apatite fission track thermochronology. The 14 outcrop samples range stratigraphically from Variscan crystalline basement through the deposits of Pennsylvanian and Permian to Triassic. Fission track data reveal significant cooling events in Mesozoic and Cenozoic. Apatite fission track data yield ages indicating Upper Permian annealing over 120°C of the Palaeozoic rocks, and Middle Triassic partial annealing (over 80°C).
Permanent Link: http://hdl.handle.net/11104/0164241
Number of the records: 1