Pregled bibliografske jedinice broj: 254365
Tectonic Implications of new paleomagnetic results from Late Cretaceous rocks of the stable part of the Adria microplate
Tectonic Implications of new paleomagnetic results from Late Cretaceous rocks of the stable part of the Adria microplate // ADRIA 2006 International Geological Congress on the Adriatic area, Abstracts
Urbino: Universita degli studi di Urbino, 2006. (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 254365 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Tectonic Implications of new paleomagnetic results from Late Cretaceous rocks of the stable part of the Adria microplate
Autori
Marton, Emoe ; Zampieri, Dario ; Ćosović, Vlasta ; Moro, Alan
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
ADRIA 2006 International Geological Congress on the Adriatic area, Abstracts
/ - Urbino : Universita degli studi di Urbino, 2006
Skup
ADRIA 2006 International Geological Congress on Adriatic Area
Mjesto i datum
Urbino, Italija, 19.06.2006. - 20.06.2006
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Paleomagnetism; tectonic; Late Cretaceous; Adria microplate
Sažetak
Adria is the largest lithospheric fragment in the Central Mediterranean region that has played a key role in the development of the surrounding mountain chains (Dinarides, Suuthern Alps, Apennines). Earlier available paleomagnetic data were suitable to characterize the displacment of Adria in a very general way and were not sufficient to supply satisfactory answers to some questions.
Izvorni jezik
Engleski
Znanstvena područja
Geologija
