Zachar Judit and M. Tóth Tivadar: Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian basin, Se Hungary) : part II. : origin and spatial relationships. In: Acta mineralogica-petrographica, (42). pp. 39-43. (2001)
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Abstract
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.
| Item Type: | Article |
|---|---|
| Journal or Publication Title: | Acta mineralogica-petrographica |
| Date: | 2001 |
| Volume: | 42 |
| ISSN: | 0365-8066 |
| Page Range: | pp. 39-43 |
| Language: | English |
| Publisher: | Department of Mineralogy, Geochemistry and Petrology, University of Szeged |
| Place of Publication: | Szeged |
| Related URLs: | http://acta.bibl.u-szeged.hu/39423/ |
| Uncontrolled Keywords: | Földtan, Kőzettan, Ásványtan |
| Additional Information: | Bibliogr.: 43. p. ; ill. ; összefoglalás angol nyelven |
| Subjects: | 01. Natural sciences 01. Natural sciences > 01.05. Earth and related environmental sciences |
| Date Deposited: | 2016. Oct. 17. 09:25 |
| Last Modified: | 2022. Aug. 09. 08:47 |
| URI: | http://acta.bibl.u-szeged.hu/id/eprint/25088 |
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