Geochemical character of amphibolites from Tisza Unit on the basis of incompatible trace elements

Pre-metamorphic origin of amphibolites and amphibolic gneisses from K6ros Complex (Eastern Tisza Unit) has been an unsolvable problem for a long time. Last year the trace element (Zr, Y, Nb, Ti, P) composition of almost 100 amphibolite samples were measured and this data base may be useful for deter...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerző: M. Tóth Tivadar
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1994
Sorozat:Acta mineralogica-petrographica 35
Kulcsszavak:Kőzettan, Ásványtan, Földtan, Geokémia
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24815
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520 3 |a Pre-metamorphic origin of amphibolites and amphibolic gneisses from K6ros Complex (Eastern Tisza Unit) has been an unsolvable problem for a long time. Last year the trace element (Zr, Y, Nb, Ti, P) composition of almost 100 amphibolite samples were measured and this data base may be useful for determining pre-metamorphic rock types and petrochemical character of amphibolites. Present examinations show that - opposite to the previous results - there were no alkaline magmatites in the area, but the rocks of both tholeiitic and calk-alkaline series were formed. The data also suggest that the original igneous rocks of amphibolic gneisses developed in an island arc, while the amphibolites' either in a fore-arc or in a back-arc basin. 
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