Ti-bearing andradite-prehnite-epidote assemblage from the Malá Fatra granodiorite and tonalite (Western Carpathians).

Abstract

Calc-silicate minerals (Ca-garnet, prehnite, epidote, titanite, actinolite) occur associated with chlorite and muscovite in Variscan tonalite and granodiorite of the Tatricum Unit in the Mali Fatra Mountains. They formed during postmagmatic cool

Keywords

• Faryad Shah Wali Ti-bearing andradite
• granitoids
• hydrothermal alteration
• Alpine metamorphism