Informace o publikaci
Clay and Závist faults as one large Variscan strike slip fault around Kozičín, Pičín and Řitka villages (Barrandian, Bohemian Massif)
| Autoři | |
|---|---|
| Rok publikování | 2013 |
| Druh | Konferenční abstrakty |
| Fakulta / Pracoviště MU | |
| Citace | |
| Popis | The Clay and the Závist faults were described as two different structures. Both these faults are steeply dipping and striking in SW-NE direction. This Paper disscuses arguments, it is evident that both faults are only parts of one sinistral strike-slip fault originated during the Lower Carboniferous. |