{"refrec":{"BRefID":211078,"RR":"<b>Tison, J.-L.; Khazendar, A.; Roulin, E.</b> (2001). A two-phase approach to the simulation of the combined isotope/salinity signal of marine ice. <i>J. Geophys. Res. 106(C12)</i>: 31387-31401. <a href=\"https://dx.doi.org/10.1029/2000JC000207\" target=\"_blank\">https://dx.doi.org/10.1029/2000JC000207</a>","BEntID":203000,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>J. Geophys. Res. 106(C12)</i>: 31387-31401. <a href=\"https://dx.doi.org/10.1029/2000JC000207\" target=\"_blank\">https://dx.doi.org/10.1029/2000JC000207</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Tison, J.-L.; Khazendar, A.; Roulin, E.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Tison, J.-L. <i>et al.</i>","Englishabstract":"A modified boundary layer box diffusion model is used to simulate the production of the combined oxygen isotope/salinity signal of a body of marine ice. The final signal is considered to be the result of fractionation and segregation processes occurring first upon the formation of frazil crystals in suspension and second during their accumulation and consolidation due to the advancement of a freezing front. The model results are compared to oxygen isotope and salinity values in a 45-m marine ice core from the Nansen Ice Shelf, Antarctica. 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