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• W1982256852 abstract "The Ekeby site, south of Stockholm, has been chosen to elucidate glaciofluvial sedimentation processes soon after the end of the Younger Dryas. Detailed lithofacies and grain-size analyses of gravel, sand and fine sediment sequences in a gravel pit reflect changes in the depositional environment. Four main facies assemblages have been distinguished. The lowermost part of the sequence was probably deposited in a subglacial conduit environment. The middle part of the sequence reflects a transition to a proglacial subaqueous environment. The upper part of the latter sequence probably occurred during increased melting of the ice. The sequence was then covered by beach gravel formed during the regression after the drainage of the Baltic Ice Lake." @default.
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• W1982256852 date "1997-01-01" @default.
• W1982256852 modified "2023-09-27" @default.
• W1982256852 title "Sedimentology of a glaciofluvial deposit at Ekeby, East Central Sweden" @default.
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• W1982256852 doi "https://doi.org/10.1016/s0277-3791(97)00021-8" @default.
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