Zachar Judit and M. Tóth Tivadar: Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian basin, Se Hungary) : part I. : myrmekite formation theories. In: Acta mineralogica-petrographica, (42). pp. 33-37. (2001)
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Abstract
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.
Item Type: | Article |
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Journal or Publication Title: | Acta mineralogica-petrographica |
Date: | 2001 |
Volume: | 42 |
ISSN: | 0365-8066 |
Page Range: | pp. 33-37 |
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. 36-37. ; 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. 08:46 |
URI: | http://acta.bibl.u-szeged.hu/id/eprint/25087 |
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