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  • borings and geophysics. The distribution of the Neogene volcanism as well as the thin crust and high heat flow found by these investigations revealed however the existence of an active young-alpine mantle arch. The area above the mantle arch subsides
  • isostatically due to the changes in density of the lithosphere and to the subsidence of the thinned crust, producing the Pannonian Basins. Finally basaltic partial melt products of the mantled arch heated gradually by the volatile emanations extrude, too
  • 1978