{"refrec":{"BRefID":241187,"RR":"<b>Violante, R.A.; Hernández-Molina, F.J.; Costa, I.P.; Schwenk, T.</b> (2014). Different styles in configuration of the contouritic drifts in the northern sector of the Argentine Continental Margin: implications in slope stability and geohazard, <b><i>in</i></b>: Van Rooij, D. <i>et al.</i> (Ed.) <i>Book of Abstracts. 2nd Deep-Water Circulation Congress: The Contourite Log-book. Ghent, Belgium, 10-12 September 2014. VLIZ Special Publication,</i> 69: pp. 17-18","BEntID":232884,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Van Rooij, D. <i>et al.</i> <i>Book of Abstracts. 2nd Deep-Water Circulation Congress: The Contourite Log-book. Ghent, Belgium, 10-12 September 2014. VLIZ Special Publication,</i> 69: pp. 17-18","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Violante, R.A.; Hernández-Molina, F.J.; Costa, I.P.; Schwenk, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Violante, R.A. <i>et al.</i>","Englishabstract":"The northern sector of the Argentine Continental Margin includes areas with significant differences in the morphosedimentary configuration of the contouritic drifts. In the northernmost part (MP area) they are represented by relatively continuous deposits not deeply affected by gravity downslope processes, whereas in the southernmost part (BB area) they are discontinuous and highly dissected by mass-transport and turbiditic deposits. 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