Pregled bibliografske jedinice broj: 7522
Tectonic Structure of the Island of Hvar (Southern Croatia)
Tectonic Structure of the Island of Hvar (Southern Croatia) // Geologia Croatica, 50 (1997), 1; 57-77 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 7522 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Tectonic Structure of the Island of Hvar (Southern Croatia)
Autori
Marinčić, Stanko
Izvornik
Geologia Croatica (1330-030X) 50
(1997), 1;
57-77
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
Kinematics of deformation; Tectonic phases; Island of Hvar; Croatia
Sažetak
Structural deformation of the island of Hvar allows three tangential tectonic phases to be determined: the Laramian (F I), the Pyrenean (F II) and the Neotectonic phase (F III). Preserved relics of Laramian and Pyrenean folds with intact structural elements, indicates that the Neotectonic orientation of structures (E-W) is a consequence of refolding of the older structural fabric, rather than horizontal rotation.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Citiraj ovu publikaciju:
Časopis indeksira:
- Scopus