Naslov
Stable Adria and the External Dinarides: Tectonic Models in the Context of Jurassic-Cretaceous Paleomagnetic Results

Autori
Marton, Emoe ; Ćosović, Vlasta ; Moro, Alan

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
Zbornik radova, XVI Kongres geologa Srbije / Cvetković, Vladica - Beograd : Srpsko geološko društvo, 2014, 61-62

ISBN
978-86-86053-14-5

Skup
XVI Kongres geologa Srbije

Mjesto i datum
Donji Milanovac, Srbija, 22.05.2014. - 25.05.2014

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
Paleomagetism; Stable Adria; External Dinarides; Mesozoic; tectonic models; rotations

Sažetak
Adria is a crustal block of African origin, playing an important role in the geodynamic history of the Central Mediterraneans s.l. It comprises the gently deformed "autochthonous" core of the thrusted and folded External Dinarides, the Apennines and the Southern Alps. A powerful method to reveal possible relative movements between the core and the margins and within each of the margins is paleomagnetism, which can provide quantitative constraints about vertical axis rotations and latitudinal displacement. From authchtonous Adria represented by stable Istria and the Adige embayment paleomagnetic results from 100 geographically distributed localities were evaluated and a reference frame was constructed which characterizes the displacements of stable Adria during Tithonian-Eocene times. Tectonic models published by Herak (1986), Pamić et al. (1998), Tari (2002), Ustaszewski et al. (2008) ad Korbar (2009) were tested against paleomagnetic data with the conclusion, that the fit is the best with the model by Tari who considered the Adriatic islands as the imbricated margin of Adria which is overridden by the fold and thrust belt of the Dinaricum.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

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