Penninic ophiolites at the eastern margin of the Eisenberg-group (Felsőcsatár, W-Hungary)
At the Eastern termination of the Alps there are various greenstones of basaltic origin, ullramafitites and a meta-ultrabasic rocks exposed in the tectonic windows of the Eisenberg-Group. The paper gives detailed description of the mineralogy and mineral chemistry of this rock suite.
Elmentve itt :
| Szerző: | |
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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/24743 |
| Tartalmi kivonat: | At the Eastern termination of the Alps there are various greenstones of basaltic origin, ullramafitites and a meta-ultrabasic rocks exposed in the tectonic windows of the Eisenberg-Group. The paper gives detailed description of the mineralogy and mineral chemistry of this rock suite. |
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| Terjedelem/Fizikai jellemzők: | 5-9 |
| ISSN: | 0365-8066 |