I am curious about fossil subduction zones. Which subsurface processes lead to the formation of metamorphic soles or blueschists and how can parts of these deeply evolved rocks be exhumed? How do volatiles from the subducted plate influence the mantle? Which role does serpentinisation of ultramafics play during exhumation? And mostly, how do these mechanisms implement as textures in rocks? To better understand this at various spatial scales, mapping and micro-scale analyses became the foundation of my work. During my masters I worked on the metamorphic sole of the Mirdita Ophiolite in Albania, whereas now I am focused on the evolution of granulites from the Saxonian Granulite massif as well as the blueschist-facies metamorphic Yuli Belt in Taiwan.