id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-747	Žibret, Lea; Vrabec, Marko	Paleostress and kinematic evolution of the orogen-parallel NW-SE striking faults in the NW External Dinarides of Slovenia unraveled by mesoscale fault-slip data anaysis	2016	11	.pdf	application/pdf	7488	341	53	The main manifestation of this phase is a dextral reactivation of NW-SE-trending fault planes. Whereas the overprinting cri teria of striae on fault planes are occasionally strongly influenced by the viewpoint of the ob- server and are therefore rarely unambiguous (SPERNER & ZWEIGEL, 2010), the calcite accretionary steps that have grown inside sub-vertical grooves on this fault plane clearly indicate that the dextral sense of slip attributed to Phase 4 postdates the normal­slip episode of Phase 2 (Fig. 7 c). 3.4.	cache/gc-747.pdf	txt/gc-747.txt