Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian basin, Se Hungary) : part I. : myrmekite formation theories

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
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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