Izvorni znanstveni članak
Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range
Darko Mihljević
Sažetak
Two principal directions of mountain ridge axes in the area of NW part of Outher Dinarides have been pointed out. They are consequence of the former and most recent tectonic active phase. Also, the kinematic model of counterclockwise rotation of structures has been outlined, and recognised as the fundamental cause of main arc shaped mountain ridges. Due to the mentioned kinemtaic model, recent morphotectonic evolution of NW part of Outer Dinarides has been interpreted.
Ključne riječi
structural geomorphology; Outher Dinarides; neotectonics; counterclockwise rotation; morphostructural evolution
Hrčak ID:
84499
URI
Datum izdavanja:
1.12.1995.
Posjeta: 1.708 *