Folds in Biancone-type limestones of the Krasta-Cukali Zone (northern Albania).
Foto: Kamil Ustaszewski
Folded Upper Jurassic to Cretaceous Limestones and radiolarites (red) of the Krasta-Cukali Zone north of Komani reservoir (northern Albania).
Foto: Kamil Ustaszewski
Cleavage refraction in rocks of the Durmitor Flysch Unit (Montenegro).
Foto: Kamil Ustaszewski
Ptygmatic folds in a quartzitic layer within carbonatic host rock. Note that shortening in the fold hinges is accommodated by small brittle faults. Krasta-Cukali Zone, northern Albania.
Foto: Kamil Ustaszewski
Pencil cleavage in a marly flysch of the Krasta-Cukali Zone (northern Albania). Such pencil cleavage typically developes close to fold hinges where the layering and cleavage include high angles and form the elongated planes of the rock fragments.
Foto: Kamil Ustaszewski
Tight to isoclinal folds in marble (near Osina, Rhodopes, S Bulgaria).
Foto: Jan Pleuger
Polyphase deformation in Ordovician schist (near Bosilegrad, SE Serbia). The first penetrative cleavage (subvertical) and a second, sporadic one (subhorizontal) are affected by folding with axial plane traces trending from bottom left to top right.
Foto: Jan Pleuger
Folds in contact-metamorphic Sediments (Kopaonik Mt., S Serbia)
Foto: Jan Pleuger
Kink faults nucleated along conjugate faults in metasediment (Kopaonik Mt., S Serbia).
Foto: Jan Pleuger
Crenulation cleavage in metasandstones, overprinting an earlier foliation. Mukua River valley, Central Range, eastern Taiwan.
Foto: Kamil Ustaszewski
Crenulated pelitic schists showing prominent crenulation lineations. MuKua Hsi Valley, Central Range, Eastern Taiwan.
Foto: Kamil Ustaszewski
Refold structures in calcite marble, Taroko gorge, Eastern Taiwan.
Folds in Biancone-type limestones of the Krasta-Cukali Zone (northern Albania).Foto: Kamil Ustaszewski
Folded Upper Jurassic to Cretaceous Limestones and radiolarites (red) of the Krasta-Cukali Zone north of Komani reservoir (northern Albania).Foto: Kamil Ustaszewski
Cleavage refraction in rocks of the Durmitor Flysch Unit (Montenegro).Foto: Kamil Ustaszewski
Ptygmatic folds in a quartzitic layer within carbonatic host rock. Note that shortening in the fold hinges is accommodated by small brittle faults. Krasta-Cukali Zone, northern Albania.Foto: Kamil Ustaszewski
Pencil cleavage in a marly flysch of the Krasta-Cukali Zone (northern Albania). Such pencil cleavage typically developes close to fold hinges where the layering and cleavage include high angles and form the elongated planes of the rock fragments.Foto: Kamil Ustaszewski
Tight to isoclinal folds in marble (near Osina, Rhodopes, S Bulgaria).Foto: Jan Pleuger
Polyphase deformation in Ordovician schist (near Bosilegrad, SE Serbia). The first penetrative cleavage (subvertical) and a second, sporadic one (subhorizontal) are affected by folding with axial plane traces trending from bottom left to top right.Foto: Jan Pleuger
Folds in contact-metamorphic Sediments (Kopaonik Mt., S Serbia)Foto: Jan Pleuger
Kink faults nucleated along conjugate faults in metasediment (Kopaonik Mt., S Serbia).Foto: Jan Pleuger
Crenulation cleavage in metasandstones, overprinting an earlier foliation. Mukua River valley, Central Range, eastern Taiwan.Foto: Kamil Ustaszewski
Crenulated pelitic schists showing prominent crenulation lineations. MuKua Hsi Valley, Central Range, Eastern Taiwan.Foto: Kamil Ustaszewski
Refold structures in calcite marble, Taroko gorge, Eastern Taiwan.Foto: Kamil Ustaszewski