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Detailed seismic stratigraphy of Lago Puyehue: implications for the mode and timing of glacier retreat in the Chilean Lake District
Authors:Katrien Heirman  Marc De Batist  Francois Charlet  Jasper Moernaut  Emmanuel Chapron  Robert Brümmer  Mario Pino  Roberto Urrutia
Institution:1. Renard Centre of Marine Geology (RCMG), Department of Geology and Soil Science, Universiteit Gent, Krijgslaan 281 S8, B‐9000 Gent, Belgium;2. Geological Institute, ETH Zürich, Zürich, Switzerland;3. Instituto de Geociencias, Universidad Austral de Chile, Valdivia, Chile;4. EULA, Universidad de Concepcion, Concepción, Chile
Abstract: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. A timing discrepancy between the in‐lake ages of a sediment core and the outer‐lake ages of moraine deposits (re)opens the discussion on the timing of deglaciation in the Southern Hemisphere. Copyright © 2011 John Wiley & Sons, Ltd.
Keywords:Lago Puyehue  Chilean Lake District  seismic stratigraphy  lake sediments  deglaciation
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