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- W2022682159 abstract "Abstract Combination of recent seismic profiles obtained along the South Cretan continental margin with previously published data, has provided a basis for mapping the overall structure of this portion of the active Hellenic Margin. Two sectors are distinguished. From western Crete to 25° east, the continental slope is crossed by post late Miocene extensional features creating a series of sedimental marginal troughs and steep basement ridges. The lower slope, the trench and parts of its outer slope are areas of little sedimentation (most of the sediments are trapped on the margin) and of active deformation. This area represents the eastern prolongation of the Ionian Branch (Matapan trench) of the Hellenic subduction zone and is interpreted in the light of NE-directed compression. From 25° E to eastern Crete, the geological structures of both the continental margin and the adjacent trenches differ from those to the west. This difference possibly relates to interferences between the present-day structural directions (interpreted in relation to a left-lateral transform motion) and previous trends inherited from a preceding NS compression." @default.
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- W2022682159 date "1982-10-01" @default.
- W2022682159 modified "2023-09-26" @default.
- W2022682159 title "Geological structures on the South Cretan continental margin and Hellenic Trench (eastern Mediterranean)" @default.
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- W2022682159 doi "https://doi.org/10.1016/0025-3227(82)90040-8" @default.
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