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Relief reflection of structural resgaping during the recent tectoniccaly active stage, in the north-western part of the outer Dinarides mountain range
Darko Mihljević
Puni tekst: engleski pdf 13.512 Kb
str. 5-12
preuzimanja: 470
citiraj
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. Preuzeto s https://hrcak.srce.hr/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., br. 1., 1995, str. 5-12. https://hrcak.srce.hr/84499. Citirano 23.04.2024.
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., br. 1. (1995): 5-12. https://hrcak.srce.hr/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.), str. 5-12. Preuzeto s: https://hrcak.srce.hr/84499 (Datum pristupa: 23.04.2024.)
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 [pristupljeno 23.04.2024.];30.(1.):5-12. Dostupno na: https://hrcak.srce.hr/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., br. 1., str. 5-12, 1995. [Online]. Dostupno na: https://hrcak.srce.hr/84499. [Citirano: 23.04.2024.]
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
https://hrcak.srce.hr/84499
Datum izdavanja:
1.12.1995.
Podaci na drugim jezicima:
hrvatski
Posjeta: 1.188
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