{"refrec":{"BRefID":285544,"RR":"<b>Duperret, A.; Raimbault, C.; Le Gall, B.; Authemayou, C.; Van Vliet-Lanoë, B.; Regard, V.; Dromelet, E.; Vandycke, S.</b> (2016). High-resolution onshore-offshore morpho-bathymetric records of modern chalk and granitic shore platforms in NW France. <i>C. r. Géosci. 348(6)</i>: 422-431. <a href=\"https://dx.doi.org/10.1016/j.crte.2015.06.005\" target=\"_blank\">https://dx.doi.org/10.1016/j.crte.2015.06.005</a>","BEntID":277569,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>C. r. Géosci. 348(6)</i>: 422-431. <a href=\"https://dx.doi.org/10.1016/j.crte.2015.06.005\" target=\"_blank\">https://dx.doi.org/10.1016/j.crte.2015.06.005</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Duperret, A.; Raimbault, C.; Le Gall, B.; Authemayou, C.; Van Vliet-Lanoë, B.; Regard, V.; Dromelet, E.; Vandycke, S.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Duperret, A. <i>et al.</i>","Englishabstract":"Modern shore platforms developed on rocky coasts are key areas for understanding coastal erosion processes during the Holocene. This contribution offers a detailed picture of two contrasted shore-platform systems, based on new high-resolution shallow-water bathymetry, further coupled with aerial LiDAR topography. Merged land-sea digital elevation models were achieved on two distinct types of rocky coasts along the eastern English Channel in France (Picardy and Upper-Normandy: PUN) and in a NE Atlantic area (SW Brittany: SWB) in NW France. About the PUN case, submarine steps, identified as paleo-shorelines, parallel the actual coastline. Coastal erosive processes appear to be continuous and regular through time, since mid-Holocene at least. In SWB, there is a discrepancy between contemporary coastline orientation and a continuous step extending from inland to offshore, identified as a paleo-shoreline. 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