Tertiary counterclockwise rotation of Adria as evidenced by new paleomagnetic data from Istria and NW Dinarids (CROSBI ID 739114)
Prilog sa skupa u časopisu | izvorni znanstveni rad
Podaci o odgovornosti
Marton, Emoe ; Drobne, Katica ; Ćosović, Vlasta
engleski
Tertiary counterclockwise rotation of Adria as evidenced by new paleomagnetic data from Istria and NW Dinarids
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.
Counterclockwise rotation; Istria; NW Dinarids; Eocene
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
nije evidentirano
Podaci o prilogu
C15-x.
1998.
nije evidentirano
objavljeno
Podaci o matičnoj publikaciji
Podaci o skupu
Nepoznat skup
ostalo
29.02.1904-29.02.2096
