Tertiary counterclockwise rotation of Adria as evidenced by new paleomagnetic data from Istria and NW Dinarids (CROSBI ID 739114)
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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
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Podaci o prilogu
C15-x.
1998.
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29.02.1904-29.02.2096