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- W2081472723 abstract "The tectonically active South Evvoikos Gulf forms the submerged part of a young basin produced by Neogene fragmentation of the Hellenides, so furnishing an opportunity to study the earliest stages of an extensional rift. Reflection profiles show three seismo-stratigraphic units: a thin Holocene unit A, a thick Late and Middle Pleistocene unit B, and a deformed Mesozoic-Cenozoic basal unit C. In the eastern Gulf, at least seven alternatingly stratified and acoustically transparent subunits are related to Pleistocene sea-level changes that episodically isolated the Gulf. Correlation with the global eustatic sea-level curve indicates that deposition in the Gulf, formed by southeastward divergence of its northern and southern boundary faults, began during the last million years. Subsequent glacio-eustatic sea-level changes superimposed major variations in depositional conditions on long-term subsidence. Lack of Pleistocene marine beds on the adjacent land implies that a high rate of subsidence confined lacustrine and marine deposition to the basin itself." @default.
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- W2081472723 date "1991-05-01" @default.
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- W2081472723 title "Sea-level changes and tectonics in the Quaternary extensional basin of the South Evvoikos Gulf, Greece" @default.
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- W2081472723 doi "https://doi.org/10.1111/j.1365-3121.1991.tb00147.x" @default.
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