Myrmekite-bearing gneiss from the Szeghalom dome (Pannonian Basin SE Hungary). Part 1.: Myrmekit formation theories
Szerző:
Dr. M. Tóth Tivadar
Zachar Judit
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.
acta2001, myrmekite, orthogneiss, Pannonian Basin
