Evolution models of two flysch basins: The Northern Carpathians and the Southern Apennines

摘要: Abstract The geological evolution of the external domains Northern Carpathians and Southern Apennines is compared two models flysch basins are proposed. first, related to a tensile stage orogeny, applied only Carpathian area during Cretaceous; latter, compressive stage, present in both areas Cenozoic. different evolutions have counterparts present-day continental margin thinning crust controls sedimentation first model and, subduction along mobile plate junctions, enables accumulation deposits trench-like take place.