{"refrec":{"BRefID":211583,"RR":"<b>Heirman, K.; De Batist, M.; Charlet, F.; Moernaut, J.; Chapron, E.; Brümmer, R.; Pino, M.; Urrutia, R.</b> (2011). Detailed seismic stratigraphy of Lago Puyehue: implications for the mode and timing of glacier retreat in the Chilean Lake District. <i>J. Quaternary Sci. 26(7)</i>: 665-674. <a href=\"http://dx.doi.org/10.1002/jqs.1491\" target=\"_blank\">dx.doi.org/10.1002/jqs.1491</a>","BEntID":203504,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Quaternary Sci. 26(7)</i>: 665-674. <a href=\"https://dx.doi.org/10.1002/jqs.1491\" target=\"_blank\">https://dx.doi.org/10.1002/jqs.1491</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Heirman, K.; De Batist, M.; Charlet, F.; Moernaut, J.; Chapron, E.; Brümmer, R.; Pino, M.; Urrutia, R.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Heirman, K. <i>et al.</i>","Englishabstract":"Lago Puyehue is a glacigenic lake in the Chilean Lake District (40°S) with a complex deglaciation history. A detailed seismic–stratigraphic study of its sedimentary infill indicates a much earlier retreat of the glacier from the Lago Puyehue basin than the neighbouring glacier from the Lago Rupanco basin. Because of their close proximity, Rupanco meltwater streams played an important part in the depositional processes of Lago Puyehue. 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