Naslov
Ore deposits of Central Europe

Autori
Harald G. Dill, Reinhard Sachsenhofer, Pavol Grecula, Tibor Sasvári, Ladislav A. Palinkaš, Sibila Borojević Šoštarić, Sabina Strmić Palinkaš, Walter Prochaska, Giorgio Garuti, Federica Zaccarini, Didier Arbouille and Markus Schulz

Vrsta, podvrsta i kategorija rada
Radovi u zbornicima skupova, cjeloviti rad (in extenso), znanstveni

Izvornik
Proceedings of the 12th Quadrennial IAGOD (International Association of the Genesis of Ore Deposits) Symposium 2006 / - Moskva, 2006

Skup
12th Quadrennial IAGOD (International Association of the Genesis of Ore Deposits) Symposium 2006

Mjesto i datum
Moskva, Ruska Federacija, 21.08.2006. - 24.08.2006

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
classification; ore deposits; Central Europe

Sažetak
A classification of non-metallic and metallic deposits as well as energy resources has been performed for Central Europe covering an area from eastern France to western Russia and from southern Denmark to northern Italy and a time span from the late Proterozoic to the Recent. The most important deposits, excluding construction raw materials were shown on a map on the scale 1: 2 500 000. The area covers the boundary between the Variscan and Alpine metallo-tectonic units which host some of the most well-known deposits on earth, e.g. Rammelsberg (D), Kupferschiefer (D, PL), Bleiberg (A), Jáchymov (CZ), Idrija (SLO), Kremnica (SK), Les Baux (F). Many oft them have significantly contributed to the understanding of the origin of similar deposits elsewhere in the world or used as type localities for classification in the field of metal deposits. Apart from the base metal deposits in Poland, it is mainly coal, salt and a wide range of non-metallic commodities which render Central Europe to rank today high up in the list of raw material producers even by world standards. The Variscan metallogenesis in Central Europe outside the Alps with predominantly granitophile elements is denominated as an "ensialic metallogenesis” , whereas the Alpine successor shows all the hallmarks of an "ensimatic metallogenesis". Part of the Variscan metallotect was re-activated during Alpine metallogenesis and incorporated into the Alpine metallotect.

Izvorni jezik
Engleski

Znanstvena područja
Geologija

POVEZANOST RADA