Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian basin, Se Hungary) part II. : origin and spatial relationships /
The metamorphic basement of the Pannonian Basin consists essentially of diverse types of amphibolite and gneiss. Due to the rather complicated structural evolution since the Variscan orogeny, the basement is at present a mosaic of crystalline blocks of incompatible evolution. That is why an exact id...
Elmentve itt :
| Szerzők: | |
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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/25088 |
| Tartalmi kivonat: | The metamorphic basement of the Pannonian Basin consists essentially of diverse types of amphibolite and gneiss. Due to the rather complicated structural evolution since the Variscan orogeny, the basement is at present a mosaic of crystalline blocks of incompatible evolution. That is why an exact identification of each rock type is crucial for being able to correlate wells spatially. Myrmekitic feldspar is an important constituent of one gneiss type, which is inferred to be of igneous origin. The orthogneiss zone seems to be an extensive part of the basement. |
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| Terjedelem/Fizikai jellemzők: | 39-43 |
| ISSN: | 0365-8066 |