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• W2076043290 abstract "Data collected during the DIAPISAR Cruise (Nov. 1990) using the French deep-towed side-scan-sonar (S.A.R.) are presented. These data provide clear evidence of recent tectonic activity in the southern part of the Barbados accretionary prism. Many markers as linear lineaments or ‘sigmoidal features’ which are observed on diagenetically indurated sea-floor are the surficial traces of faults or folds and networks of conjugate fractures where fluids are released through the structures and provide very active venting. These markers can serve as a basis for detailed mapping of some of the tectonic structures and for an analysis of their kinematic evolution. Their geometry suggests the occurrence of reworked folds and shear zones. This domain is affected by abundant clay-diapiric tectonics due to the interaction between: (1) the sedimentological context characterized by the important terrigenous supplies coming from the Orinoco River and building a wide prodelta in which levels of clay supersaturated in water can act as decollement layers, and (2) the geodynamic context of the area situated in the connection zone of three different types of margins. The data presented show that, on the eastern end of the South Caribbean wrench fault system, shear stresses can rework either ‘en echelon’ folds associated with this system or compressional structures due to subduction. The most recent structures seem largely due to the influence of shearing and correspond to transpressive or transtensive deformations rather than pure compressional structures." @default.
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• W2076043290 date "1998-01-01" @default.
• W2076043290 modified "2023-10-18" @default.
• W2076043290 title "Recent tectonic activity in the South Barbados prism Deep-towed side-scan sonar imagery" @default.
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• W2076043290 doi "https://doi.org/10.1016/s0040-1951(97)00164-9" @default.
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