M. SOCOLESCU, D. POPOVICI, M. VISARION and V. ROSCA
In concordance with the isostatic anomalies, the density of the geological
formations and the assumption that the intermediate layer has a uniform thickness,
was drawn the form of the Mohorovicic discontinuity under the Romanian territory.
This discontinuity presents an important inflection under the Eastern Carpathians
and another smaller inflexion, parallel to the first and passing across the
Apuseni Mountains. Both of them are parallel with the trend of the known
Craistides from the region of Moravian Valley and Western Balkans. These
inflexions are correlated with the magnetic phenomena of the orogenic belts
and form the support of the metallogenetic provinces.