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Authors | |
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Year of publication | 2011 |
Type | Article in Periodical |
Magazine / Source | Trabajos de Geología |
MU Faculty or unit | |
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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