You are here:
Publication details
Touching the Detachment (Ockov Fault, Barrandian, Czech Republic)
Authors | |
---|---|
Year of publication | 2008 |
Type | Conference abstract |
MU Faculty or unit | |
Citation | |
Description | The Prague Synform (Ordovician to Devonian) was folded and thrusted during the Variscan orogeny. The paper is focused on one of the 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: |