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- W2058730552 abstract "A 147 cm core from the Gulf of Kavalla on the northern Aegean shelf displays two different lithologies separated by an erosional contact. The upper part (0–128 cm) consists of clayey silt to silty clay grading into silty sand and represents a neritic to nearshore marine environment. The lower section (128–147 cm) is a stiff calcareous mudstone with scattered microcrystalline calcite nodules, and probably represents part of a subaerial soil horizon (Bca). Seismic data indicate that at this location the unconformity between the late glacial subaerial surface and the overlying post-glacial transgressive deposits occurs at a depth of 150 cm, and has apparently been sampled by the core." @default.
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- W2058730552 date "1988-06-01" @default.
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- W2058730552 title "Late Pleistocene unconformity in the Gulf of Kavalla, northern Aegean, Greece" @default.
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- W2058730552 doi "https://doi.org/10.1016/0025-3227(88)90017-5" @default.
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