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- W2091046654 abstract "Die Chronologie des Gletscherruckzuges vom Letzteiszeitlichen Maximum ist in den Schweizer Alpen und im Alpenvorland ungeniigend erfasst. Die vorhandenen 14C-Datierungen an postglazialen Basis-sedimenten weisen auf zeitgleichen Eiszerfall um 14'000 y BP sowohl im Vorland als auch in den Alpen hin (Fig. 1). Offene Fragen zu einem solchen gleichzeitigen Wegschmelzen des alpinen Eises sind kurz diskutiert." @default.
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- W2091046654 date "1988-01-01" @default.
- W2091046654 modified "2023-09-27" @default.
- W2091046654 title "The deglaciation of the Swiss-Alps : a paleoclimatic event with chronological problems" @default.
- W2091046654 doi "https://doi.org/10.3406/quate.1988.1875" @default.
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