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- W2339841036 abstract "Puerto Rico is located within a zone of tectonic transition between mainly east-west, North America–Caribbean strike-slip motion to the west in Hispaniola and east-northeast–oriented underthrusting to the east beneath the Lesser Antilles island arc. Various models and tectonic mechanisms have been proposed for the Neogene to present-day deformation of southern Puerto Rico, its island margin, and the Muertos trench by previous workers that include normal, thrust, and strike-slip faulting accompanied by large-scale rotations. In this study, we present the results of a regional study integrating onland mapping of striated fault surfaces in rocks ranging in age from Oligocene to possibly as young as earliest Pliocene, and offshore mapping of faults deforming the uppermost sediments beneath the seafloor." @default.
- W2339841036 created "2016-06-24" @default.
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- W2339841036 date "2005-01-01" @default.
- W2339841036 modified "2023-10-15" @default.
- W2339841036 title "Neotectonics of southern Puerto Rico and its offshore margin" @default.
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- W2339841036 doi "https://doi.org/10.1130/0-8137-2385-x.173" @default.
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