Touching the Detachment

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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.
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