ÉTUDES PÉTROGÉNÉTIQUES ET PÉTROMAGNÉTIQUES DANS LA REGION DE BAIA DE ARIES

par TOMA PETRE GHITULESCU1, DRAGOMIR ROMANESCU2, GEORGE PITULEA1,
IOANA GHITULESCU1, ANCA GEORGESCU2 et TITU NESTIANU2
1IGPSMS, Bucarest
2Institut de Géologie et Géophysique, Bucarest

Petrographic and petromagnetic correlation studies helped solving some interesting problems concerning the Neogen magmatism in the Baia de Aries district. In a volcanic complex the natural remanent magnetization values are much greater in enrooted bodies (necks, subvolcans, dykes, apophysis) than in lavas and pyroclastics. They are also much greater in the central part of a neck than on its borders. The morphology of the Z isodynamics reflects the inner constitution of a subvolcanic body. The magnetic parameters of the andesite are not affected by the propylitic transformation but are very diminished with potassium hydrothermalisation; especially the natural remanent magnetization diminishes much quicker than the magnetic susceptibility.