Structural evolution of mylonitized gneiss zone from the Northern Flank of the Szeghalom Dome (Pannonian Basin, Se Hungary)
Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and structural evolution in the area of the Szeghalom high. Here evolution of a large-scale shear zone from the northern flank of the uplifted dome is studied. Textural relics suggest that the original rock ty...
Elmentve itt :
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| Dokumentumtípus: | Cikk |
| Megjelent: |
Department of Mineralogy, Geochemistry and Petrology, University of Szeged
Szeged
2001
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| Sorozat: | Acta mineralogica-petrographica
42 |
| Kulcsszavak: | Földtan, Kőzettan, Ásványtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/25091 |
| Tartalmi kivonat: | Metamorphic basement of the Pannonian Basin consists of blocks of incompatible metamorphic and structural evolution in the area of the Szeghalom high. Here evolution of a large-scale shear zone from the northern flank of the uplifted dome is studied. Textural relics suggest that the original rock type was orthogneiss widespread in the surroundings. Deformation produced a wide (over 200 m) shear zone with welldeveloped mylonite in the centre. We show, that the deformation followed the last progressive metamorphic event of the basement. |
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| Terjedelem/Fizikai jellemzők: | 59-64 |
| ISSN: | 0365-8066 |