Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian basin, Se Hungary) part I. : myrmekite formation theories /
Myrmekite is a common textural feature in many magmatic and metamorphic rock types. Nevertheless, there are several theories concerning its genesis; myrmekite may form by igneous crystallization, solid state exsolution, progressive or retrograde metamorphism, metasomatism or even as a result of comp...
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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/25087 |
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| 008 | 161017s2001 hu o 0|| eng d | ||
| 022 | |a 0365-8066 | ||
| 040 | |a SZTE Egyetemi Kiadványok Repozitórium |b hun | ||
| 041 | |a eng | ||
| 100 | 1 | |a Zachar Judit | |
| 245 | 1 | 0 | |a Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian basin, Se Hungary) |h [elektronikus dokumentum] : |b part I. : myrmekite formation theories / |c Zachar Judit |
| 260 | |a Department of Mineralogy, Geochemistry and Petrology, University of Szeged |b Szeged |c 2001 | ||
| 300 | |a 33-37 | ||
| 490 | 0 | |a Acta mineralogica-petrographica |v 42 | |
| 520 | 3 | |a Myrmekite is a common textural feature in many magmatic and metamorphic rock types. Nevertheless, there are several theories concerning its genesis; myrmekite may form by igneous crystallization, solid state exsolution, progressive or retrograde metamorphism, metasomatism or even as a result of complicated deformation mechanisms. In this paper a brief compilation of these models is given and classified by myrmekite forming processes instead of rock types or minerals involved. | |
| 650 | 4 | |a Természettudományok | |
| 650 | 4 | |a Föld- és kapcsolódó környezettudományok | |
| 695 | |a Földtan, Kőzettan, Ásványtan | ||
| 700 | 0 | 2 | |a M. Tóth Tivadar |e aut |
| 856 | 4 | 0 | |u http://acta.bibl.u-szeged.hu/25087/1/mineralogica_042_033-037.pdf |z Dokumentum-elérés |