| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 9462923 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2005 | 36 Pages |
Abstract
Restorated palaeotopography indicates the existence of two orographically separated drainage systems in the KRB. The eastern part of the Kladno-RakovnÃk Basin was drained to the NW, possibly to the North Variscan Foredeep, whilst its western part was probably drained through a central tectonic valley to the south-southwest to the Radnice and PlzeÅ basins and then further SSW, perhaps to the Naab Basin in SE Bavaria. The KRB was probably located about 1000 m above the Carboniferous sea level.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
Stanislav Opluštil,