Original scientific paper
Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range
Darko Mihljević
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cite
APA 6th Edition
Mihljević, D. (1995). Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range. Acta Geographica Croatica, 30. (1.), 5-12. Retrieved from https://hrcak.srce.hr/index.php/84499
MLA 8th Edition
Mihljević, Darko. "Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range." Acta Geographica Croatica, vol. 30., no. 1., 1995, pp. 5-12. https://hrcak.srce.hr/index.php/84499. Accessed 21 Nov. 2024.
Chicago 17th Edition
Mihljević, Darko. "Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range." Acta Geographica Croatica 30., no. 1. (1995): 5-12. https://hrcak.srce.hr/index.php/84499
Harvard
Mihljević, D. (1995). 'Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range', Acta Geographica Croatica, 30.(1.), pp. 5-12. Available at: https://hrcak.srce.hr/index.php/84499 (Accessed 21 November 2024)
Vancouver
Mihljević D. Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range. Acta Geographica Croatica [Internet]. 1995 [cited 2024 November 21];30.(1.):5-12. Available from: https://hrcak.srce.hr/index.php/84499
IEEE
D. Mihljević, "Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range", Acta Geographica Croatica, vol.30., no. 1., pp. 5-12, 1995. [Online]. Available: https://hrcak.srce.hr/index.php/84499. [Accessed: 21 November 2024]
Abstract
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.
Keywords
structural geomorphology; Outher Dinarides; neotectonics; counterclockwise rotation; morphostructural evolution
Hrčak ID:
84499
URI
https://hrcak.srce.hr/84499
Publication date:
1.12.1995.
Article data in other languages:
croatian
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