Pregled bibliografske jedinice broj: 100204
Preliminary evidence of impact origin of the Krk-breccia, Island of Krk, eastern Adriatic
Preliminary evidence of impact origin of the Krk-breccia, Island of Krk, eastern Adriatic // Abstracts and Proceedings of Norwegian Geological Society 1 / Smelror, M. ; Dypvik, H. ; Tsikalas, F. (ur.).
Trondheim: Tapir Academic Press, 2001. str. 59-61 (poster, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 100204 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Preliminary evidence of impact origin of the Krk-breccia, Island of Krk, eastern Adriatic
Autori
Marjanac, Tihomir ; Tomša, Ana Marija ; Marjanac, Ljerka
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
Abstracts and Proceedings of Norwegian Geological Society 1
/ Smelror, M. ; Dypvik, H. ; Tsikalas, F. - Trondheim : Tapir Academic Press, 2001, 59-61
Skup
7th Workshop of the ESF IMPACT Programme: Submarine craters and ejecta-crater correlation and Icy impacts and icy targets, Svalbard 2001
Mjesto i datum
Svalbard, Norveška, 29.08.2001. - 03.09.2001
Vrsta sudjelovanja
Poster
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Adriatic; Krk island; breccia; impact structure
Sažetak
Krk-breccia of northern Dalmatian Krk Island probably represents an impact crater infill which was created by transient crater slope failures and debris back-fall which followed soon after the impact. Breccia distribution indicates that it is confined to a crater of estimated diametre of 14 km, and characterized by modern subsidence of annular ring, which encircles a low central uplift. The age of the Krk-breccia is poorly confined and it can be (at present) only estimated as post-Lutetian.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
