Schubert Félix and M. Tóth Tivadar: Structural evolution of mylonitized gneiss zone from the Northern Flank of the Szeghalom Dome (Pannonian Basin, Se Hungary). In: Acta mineralogica-petrographica, (42). pp. 59-64. (2001)
Preview |
Cikk, tanulmány, mű
mineralogica_042_059-064.pdf Download (4MB) | Preview |
Abstract
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.
| Item Type: | Article |
|---|---|
| Journal or Publication Title: | Acta mineralogica-petrographica |
| Date: | 2001 |
| Volume: | 42 |
| ISSN: | 0365-8066 |
| Page Range: | pp. 59-64 |
| 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.: p. 63-64. ; 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. 08:43 |
| URI: | http://acta.bibl.u-szeged.hu/id/eprint/25091 |
Actions (login required)
 |
View Item |
