The Žužemberk Fault (pronounced [ˈʒuːʒɛmbɛɾk]; Slovene: Žužemberški prelom) is a fault in Slovenia.[1][2] The Upper Carniola Basin may have formed as a pull-apart basin between the dextral Žužemberk and Sava faults during the Quaternary.[3]
References
edit- ^ Šebela, Stanka; Gosar, Andrej; Košťák, Blahoslav; Stemberk, Josef (2005). "Active tectonic structures in the W part of Slovenia–Setting of micro-deformation monitoring net". Acta Geodyn. Geomater. 2.
- ^ Nicholas Pinter, ed. (2006). The Adria microplate : GPS geodesy, tectonics and hazards : [proceedings of the NATO Advanced Research Workshop on the Adria Microplate: GPS Geodesy, Tectonics and Hazards, Veszprem, Hungary, April 4-7, 2004]. Dordrecht: Springer. ISBN 978-1-4020-4233-1.
- ^ Vrabec, Marko; Pavlovčič Prešeren, Polona; Stopar, Bojan (2006). "GPS study (1996—2002) of active deformation along the Periadriatic fault system in northeastern Slovenia: tectonic model". Geologica Carpathica. 57. Retrieved 10 August 2014.
 | This Slovenian geography article is a stub. You can help Wikipedia by expanding it. |