{"refrec":{"BRefID":297960,"RR":"<b>Rebesco, M.; Larter, R.D.; Camerlenghi, A.; Barker, P.F.</b> (1996). Giant sediment drifts on the continental rise west of the Antarctic Peninsula. <i>Geo-Mar. Lett. 16(2)</i>: 65-75. <a href=\"https://dx.doi.org/10.1007/bf02202600\" target=\"_blank\">https://dx.doi.org/10.1007/bf02202600</a>","BEntID":290050,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Geo-Mar. Lett. 16(2)</i>: 65-75. <a href=\"https://dx.doi.org/10.1007/bf02202600\" target=\"_blank\">https://dx.doi.org/10.1007/bf02202600</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Rebesco, M.; Larter, R.D.; Camerlenghi, A.; Barker, P.F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Rebesco, M. <i>et al.</i>","Englishabstract":"Multichannel seismic reflection profiles from the continental rise west of the Antarctic Peninsula between 63° and 69°S show the growth of eight very large mound-shaped sedimentary bodies. MCS profiles and long-range side-scan sonar (GLORIA) images show the sea floor between mounds is traversed by channels originating in a dendritic pattern near the base of the continental slope. 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