Cretaceous and Tertiary paleomagnetic results from Istria and NW Dinarides (CROSBI ID 482130)
Prilog sa skupa u zborniku | sažetak izlaganja sa skupa
Podaci o odgovornosti
Marton, Emoe ; Drobne, Katica ; ćosović, Vlasta
engleski
Cretaceous and Tertiary paleomagnetic results from Istria and NW Dinarides
The "autochtonous" Istria palemagnetic data support the existance of an Adriatic microplate rotating counterclockwise with respect to both the African and European plates, in the post-Eocene times. The "paraautochtonous" Dinaric chain may consists of three parts: Udine-Divača partand Vipava valley rotating clockwise, while southern trust sheets must rotated together with the Adriatic microplate.
Istria; NW Dinarides; Adriatic microplate; Cretaceous; Tertiary; Counterclockwise rotation
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Podaci o prilogu
502-x.
2000.
objavljeno
Podaci o matičnoj publikaciji
Zbornik radova 2. hrvatskog geološkog kongresa, Cavtat - Dubrovnik, 17-20.05.2000.
Vlahović, Igor & Biondoć, Ranko
Zagreb: Hrvatski geološki institut
Podaci o skupu
2. hrvatski geološki kongres
poster
17.05.2000-20.05.2000
Cavtat, Hrvatska
