Field views of structures of the Late Cretaceous events; (17.1) The Late Cretaceous Almopias series is affected by N110°E trending folds of the (D₃) event, refolded by B₂ fold with a strain-slip schistosity (D4 event) (location: site A5, Fig. 4B); (17.2) the Eastern Almopias radiolaritic units thrust upon the western Paikon margin and are re-faulted top-to-the-SW (location: site A9 on Fig. 4B, red arrow); (17.3) the Almopias flysch thrusts westward on the western Paikon margin (D3 event; location: site A9, fig. 4B, green arrow);17.4: the Dedeli-Rabrovo serpentinite slice thrusts the Paleogene Vardar molasse (location: Artzan basin, near Dedeli (Fig. 11).