{"refrec":{"BRefID":63470,"RR":"<b>Salomons, W.; Hofman, P.; Boelens, R.; Mook, W.G.</b> (1975). The oxygen isotopic composition of the fraction less than 2 microns (clay fraction) in recent sediments from western Europe. <i>Mar. Geol. 18(1)</i>: M23-M28. <a href=\"http://dx.doi.org/10.1016/0025-3227(75)90036-5\" target=\"_blank\">http://dx.doi.org/10.1016/0025-3227(75)90036-5</a>","BEntID":60019,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Mar. Geol. 18(1)</i>: M23-M28. <a href=\"http://dx.doi.org/10.1016/0025-3227(75)90036-5\" target=\"_blank\">http://dx.doi.org/10.1016/0025-3227(75)90036-5</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Salomons, W.; Hofman, P.; Boelens, R.; Mook, W.G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Salomons, W. <i>et al.</i>","Englishabstract":"The oxygen isotopic composition of the clay fraction in Recent argillaceous sediments in western Europe shows regional differences, the <i>d</i><sup>18</sup><sub>SMOW</sub> values varying between + 15.8 and + 21.7‰. This phenomenon is used for sediment-transport studies. In the Rhine-Meuse estuary a landward transport of marine sediments is observed. 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