Abstract
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.
Recommended Citation
Balintoni, I. and Baier, U.
(2001)
Structural Researches in the Eastern Carpathians (in Romanian),
Studia UBB Geologia
46
(1): 3-14
DOI: http://dx.doi.org/10.5038/1937-8602.46.1.1
Available at:
https://digitalcommons.usf.edu/geologia/vol46/iss1/art1
