Mineralogic and isogeothermic investigation of chemichal geodynamic functions in the kyanite quartsite between Gozluce-Duvenlik-Kockoy (Malatya)

Mineralogic and İsogeothermic Investigation of Chemichal Geodynamic Functions in The Kyanite quartsite between Gözlüce-Düvenlik-Koçköy (Malatya) In this thesis, the mineralogical, petrographical and mineral chemistry properties of Gözlüce- Düvenli-Koçköy around are examined and the petrologic proceses that has resulted in generation of these rocks and rock-forming processes are interpreted. The Disten quartsites is lens and veins within the metapelitic and psamitic rocks of the Pütürge Massif. On the basis of mineralogicalpetrographical examinations and chemichal analyses, the Kyanite quartsite contains quartz, kyanite, and muscovite as main constituents and muscovite, serisite and sulphite and oxides as a secondary minerals Geology, petrography, Raman spectroscopy, whole rock, major and trace element results reveal that kyanite quartsites derived from the fluid flow with tectonism and aluminum mobility during the uplift of metamorphic massif.