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Ravines that dissect the presumably lithified scarps bounding the seamounts may be relict features but still appear to control sediment input to gulley and channel systems in the surrounding topography. Sedimentary ridges associated with the seamounts represent anomalously thick sequences of post-Eocene material and probably result from interaction of downslope sedimentary processes and contour-following boundary currents.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Geological interpretation of combined SEABEAM, GLORIA and seismic data from Porto and Vigo seamounts, Iberian continental margin","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1984,"MonPub":null,"DateUpdate":"2012-10-24","DateCreate":"2005-11-09","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:A1984TT93400001","VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":77671,"PubliDate":1984,"Pagination":"329-363","XtraPublOfAnaID":null,"ISBN":null,"Volume":"6","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43366,"SerRR":"Marine Geophysical Researches. 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