{"refrec":{"BRefID":325307,"RR":"<b>Borisov, D.; Frey, D.; Levchenko, O.</b> (2020). Sediment waves on the Santa Catarina Plateau (western South Atlantic). <i>J. South Am. Earth Sci. 102</i>: 102698. <a href=\"https://dx.doi.org/10.1016/j.jsames.2020.102698\" target=\"_blank\">https://dx.doi.org/10.1016/j.jsames.2020.102698</a>","BEntID":318784,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>J. South Am. Earth Sci. 102</i>: 102698. <a href=\"https://dx.doi.org/10.1016/j.jsames.2020.102698\" target=\"_blank\">https://dx.doi.org/10.1016/j.jsames.2020.102698</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Borisov, D.; Frey, D.; Levchenko, O.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Borisov, D.; Frey, D.; Levchenko, O.","Englishabstract":"High-resolution seismoacoustic and multibeam data revealed a large field of sediment waves covering the Santa Catarina Plateau on the Brazilian Southern Margin. Within the field several zones were determined: a zone of large sediment waves (up to 70 m in height), a zone of smaller sediment waves (15–30 m in height) and a zone of buried sediment waves. The correlation of the seismoacoustic and multibeam data with the results of numerical modeling of bottom current velocities showed a strong influence of bottom currents on the formation of sediment waves. 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