Very low-grade metamorphism of sedimentary rocks of the Meliata unit, Western Carpathians, Slovakia: implications of phyllosilicate characteristics

Abstract

The Meliata unit represents a melange-like accretionary wedge, containing blueschist facies tectonic blocks and slices in a Triassic and Jurassic sedimentary matrix. The blueschist facies rocks are tectonic remnants of the subducted parts of the

Keywords

• Faryad Shah Wali accretionary metamorphism
• very low-grade metamorphism
• illite-white mica
• chlorite
• Western Carpathians