(1a) Field view of folds (B₁) with an eastern vergence in the HP-HT metamorphic sole below the ophiolitic Mirdita sheet, (1b) refolded by (B₂) folds with a western vergence. Folds are underlined by quartz (Q) veinlets; (2a) Structural sections of folds of the Mirdita eastern margin, (2b) that result from inversion of west dipping faults (0), thrust first top-to-the-E (arrow 1) and followed by westward folding (arrow 2) (after Godroli, 1992, modified).