Trace elements in metamorphic and granitoid rocks of the basement in the Central Danube-Tisza Interfluve (Hungary)
Trace elements of the metamorphic and granitoid rocks of the Kiskunhalas—Tazlar—Szank— Jaszszentlaszl6 region lying in the central part of the Danube—Tisza Interfluve were studied. By means of the trace element diagrams the trace element distribution of different rock types can be compared and the p...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1986
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| Sorozat: | Acta mineralogica-petrographica
28 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24747 |
| Tartalmi kivonat: | Trace elements of the metamorphic and granitoid rocks of the Kiskunhalas—Tazlar—Szank— Jaszszentlaszl6 region lying in the central part of the Danube—Tisza Interfluve were studied. By means of the trace element diagrams the trace element distribution of different rock types can be compared and the premetamorphic rocks can be identified with satisfactory approximation, as well. In the region in question the gneisses are of pelitic, the amphibolites of basis igneous origin, with high probability. Migmatitization and milonitization did not cause considerable changes in the trace element compositions of the rocks. The trace element distribution pattern of granitoids remarkably differs from that of the metamorphic rocks. Keywords: metamorphic rocks, granitoid rocks, trace element geochemistry, pedogenesis. |
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| Terjedelem/Fizikai jellemzők: | 47-55 |
| ISSN: | 0365-8066 |