Structural Researches in the Eastern Carpathians. The Alpine mesoscopic lineations in the East Carpathians metamorphics, are NW-SE orientated. A few lineations, nearly E-W orientated, could be proved as pre-Alpine in age. Within the Ditrău Massif, is conserved a pre-Alpine attitude of foliations, as frozen magmatic flow, along the metamorphic pre-Triassic fabric. The lineation directions were conditioned by the Cretaceous-Tertiary contractional elimination of the External Carpathian Flysch Basin.
Balintoni, I. and Baier, U.
Structural Researches in the Eastern Carpathians (in Romanian),
Studia UBB Geologia
Available at: https://scholarcommons.usf.edu/geologia/vol46/iss1/art1