Cuba Geological Sketch
Geochemical Solutions International, Inc. (GSI)
The structural framework of the Cuban Archipelago and its adjacent seas formed primarily as a result of the collision and subsequent subduction of the Caribbean Plate (Cretaceous Volcanic Arch or Zaza terrain) under the North American continental margin during the Late Cretaceous-Middle Eocene Laramide Orogeny (Shein et al., 1975, 1980, 1985; Tenreyro et al., 1991, 1994, SPT-CUPET, 1993; Lopez et al., 1995).
The structural framework was influenced by the isostatic adjustment and lateral displacement (through shear faults) (Shein et al., op.cit.; Iturralde, 1972, 1984: SPT-CUPET,1993; Tenreyro et al., op.cit.; Echevarria et al., 1991; Socorro et al., 1995; Sosa et al., 1998). These processes led to uplift and subsequent erosion of mountains and formation of new depocenters, giving rise to the main geological and tectonic provinces that characterize this portion of the Caribbean-Mexican region.