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Authors	ČERNÝ Jan MELICHAR Rostislav KNÍŽEK Martin JANEČKA Jiří
Year of publication	2011
Type	Article in Periodical
Magazine / Source	Trabajos de Geología
MU Faculty or unit	Faculty of Science
Citation
web	plný text
Field	Geology and mineralogy
Keywords	detachment; fault core; stratigraphic separation diagram; Barrandian; Lower Paleozoic
Description	The Prague Synform (Ordovician to Devonian) was folded and thrusted during the Variscan orogeny. This paper is focused on one of these thrusts: the Ockov Fault. The creation of a stratigraphic separation diagram and detailed study of new tunnel exposures has brought about the recognition of the eastern prolongation of the fault, as well as its flat-ramp-flat geometry and thrusting nature.
Related projects:	Interactions among the chemicals, environment and biological systems and their consequences on the global, regional and local scales (INCHEMBIOL) Strukturně geologický a paleotektonický vývoj pražské pánve Barrandienu