Publication details
Clay and Závist faults as one large Variscan strike slip fault around Kozičín, Pičín and Řitka villages (Barrandian, Bohemian Massif)
| Authors | |
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| Year of publication | 2013 |
| Type | Conference abstract |
| MU Faculty or unit | |
| Citation | |
| Description | 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. |