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The tectonics are attributed to a triple boundary created from the interplay of the southern American, Caribbean and Atlantic Plates. Deformation of the Basin is made typical by the Over Thrust Faulting. The Geological formations within the southern basin are marked by sudden and intense folding and deep seated thrust faulting of basement material. These faults are estimated to extend below 35000 ft and exhibit very concave surfaces and gentle deep roots with frequent bifurcations called splay faults. These splay faults extend as far as 10,000 feet below the ground.
In order to determine the basin type and the deformation mechanism, the information above has to be analyzed...
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