Počet záznamů: 1
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 - Abstrakt
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]
Grant CEP: GA AV ČR KJB3111305
Výzkumný záměr: CEZ:AV0Z30130516
Klíčová slova: fission track * apatite * Krkonoše Piedmont basin
Kód oboru RIV: DB - Geologie a mineralogie
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).
Trvalý link: http://hdl.handle.net/11104/0164241
Počet záznamů: 1