{"refrec":{"BRefID":13412,"RR":"<b>Beck, C.; Van Rensbergen, P.; De Batist, M.; Berthier, F.; Lallier, S.; Manalt, F.</b> (2001). The late quaternary sedimentary infill of Lake Annecy (northwestern Alps): an overview from two seismic-reflection surveys. <i>J. Paleolimnol. 25</i>: 149-161. <a href=\"http://dx.doi.org/10.1023/A:1008175728826\" target=\"_blank\">http://dx.doi.org/10.1023/A:1008175728826</a>","BEntID":13412,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>J. Paleolimnol. 25</i>: 149-161. <a href=\"http://dx.doi.org/10.1023/A:1008175728826\" target=\"_blank\">http://dx.doi.org/10.1023/A:1008175728826</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Beck, C.; Van Rensbergen, P.; De Batist, M.; Berthier, F.; Lallier, S.; Manalt, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Beck, C. <i>et al.</i>","Englishabstract":"The sedimentary fill of Lake Annecy (northwestern Alps) - related to the last glacial/post-glacial episode - was investigated through high resolution (sparker) and very high resolution (2.5 kHz) seismic-reflection surveys. A seismostratigraphic approach led to subdivision of a 150 m-thick pile (maximum thickness in axial part) into five units. Basal units (1 and 2) represent an imbrication of subglacial and glacio-lacustrine deposits, close to the grounding line of the glaciers'' fronts (respectively at the northern and southern terminations of the lake). The first acoustically well-stratified unit (3) developed during a fast retreat of the glaciers fronts far from the lake basin, and a progradational alluvial regime, with abundant underflows, in a lake larger than the present one. Unit 4 represents the progressive decrease of this clastic input mixed with the progressive development of in situ bio-induced production. As in many other alpine lakes, a topmost unit (5), relatively thin (about 8-10 m) and with a conspicuous drape configuration, is the signature of the Holocene interglacial climatic conditions with a sedimentation rate of about 1 mm/yr. On the lacustrine basin slopes, slumps and debris flow occurred mainly within Unit 3; they may be due to, either climate-induced high rate terrigenous sedimentation, or/and to a period of increased seismo-tectonic activity. 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