Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

Continuation of the Periadriatic and NW Dinaridic units in the basement of the Pannonian Basin. (CROSBI ID 469070)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa

Haas, János ; Mioč, Pero ; Pamić, Jakob ; Tomljenović, Bruno ; Árkai, Péter ; Bérczi-Makk, Anikó ; Kovács, Œándor ; Rállisch-Felgenhauer, Erzsébet ; Continuation of the Periadriatic and NW Dinaridic units in the basement of the Pannonian Basin. // 16th Congres of Carpato-Balkan Geological Association. Proceedings / xy (ur.). Beč, 1998. str. 199-x

Podaci o odgovornosti

Haas, János ; Mioč, Pero ; Pamić, Jakob ; Tomljenović, Bruno ; Árkai, Péter ; Bérczi-Makk, Anikó ; Kovács, Œándor ; Rállisch-Felgenhauer, Erzsébet ;

engleski

Continuation of the Periadriatic and NW Dinaridic units in the basement of the Pannonian Basin.

Summarising and re-evaluating of the relevant surface and subsurface data in the area of Slovenia, Croatia and Hungary, we came to the following conclusions. The concept that the Slavonian mountains belong to the Tisia Terrane is widely accepted. The Savia-Mid-Transdanubia Composite Terrane, locating between the Mid-Hungarian and the Balaton Lineaments, includes Kalnik Unit; Medvednica Unit; South Zala Unit; Julian-Savinja Unit; South Karavanke Unit.

Periadriatic-Balaton and Zagreb-Zemplen Fault; Dinarides; Alps; mixed lithologies

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o prilogu

199-x.

1998.

objavljeno

Podaci o matičnoj publikaciji

16th Congres of Carpato-Balkan Geological Association. Proceedings

xy

Beč:

Podaci o skupu

16th Congres of Carpato-Balkan Geological Association

predavanje

26.08.1998-30.08.1998

Beč, Austrija

Povezanost rada

Geologija