(a) Calcitic marble boudinage inside the Inopos reservoir (C23); (b) Intense folding in the south of Inopos reservoir (C23). Marble and amphibolite reach a vertical dip; (c) Strongly fractured dolomitic marble in the northern part of Ghlastropi hill (C24); (d) Pyroxenite boudinage inside calcitic marble, Ghlastropi hill (C24); (e) Southern skarn between amphibolite and marble in quarry C25. Fine amphibolite foliation is perpendicularly cut by epidote veins; (f) Pyroxenite with decimetric garnet clusters in the northern skarn of quarry C25; (g) Thin whitish dolomitic layers inside C32 calcitic marble; (h) Calcitic marble with centimetre-size crystals, C32.