Pregled bibliografske jedinice broj: 73389
Tertiary counterclockwise rotation of Adria as evidenced by new paleomagnetic data from Istria and NW Dinarids
Tertiary counterclockwise rotation of Adria as evidenced by new paleomagnetic data from Istria and NW Dinarids // Annales Geophysicae, 16 (1998), Suppl. I. (podatak o recenziji nije dostupan, kongresno priopcenje, znanstveni)
CROSBI ID: 73389 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Tertiary counterclockwise rotation of Adria as evidenced by new paleomagnetic data from Istria and NW Dinarids
Autori
Marton, Emoe ; Drobne, Katica ; Ćosović, Vlasta
Izvornik
Annales Geophysicae 16
(1998), Suppl. I;
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, kongresno priopcenje, znanstveni
Ključne riječi
Counterclockwise rotation; Istria; NW Dinarids; Eocene
Sažetak
Paleomagnetic study was undertaken on K/T boundary through Lutetian rocks, between the Idria fault and the southernmost promotory of Istrian peninsula. In Istria counterclockwise rotation with respect to both the African and European plates took place in post mid-Eocene time. Further to the N clockwise rotation was found.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
POVEZANOST RADA
Projekti:
119301
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Vlasta Ćosović
(autor)
