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Superposed structural styles of the Maracaibo basin, Venezuela

basin ocurred z collision and subduction But, the northeastern edge underwent an obduction ( Fig 3 E-W Section across the Icotea Structure I The oblique collision with the Caribbean plate caused a subduction under the Santa Marta Massive in Colombia, which



Tectonophysics, 125 (1986) 133-160 Elsevier Science

of the Hengchun peninsula) This obduction occurred 7 to 8 Ma before the beginning of collision These results make it possible to propose an evolutionary model for Taiwan from the Oligocene to the Recent, with the different phases of a collision between a volcanic arc and a passive margin THE GEOLOGICAL AND GEODYNAMIC FRAMEWORK

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