{"refrec":{"BRefID":2986,"RR":"<b>Jacobs, P.; De Batist, M.</b> (1996). Sequence stratigraphy and architecture on a ramp-type continental shelf: the Belgian Palaeogene, <b><i>in</i></b>: De Batist, M. <i>et al.</i> (Ed.) <i>Geology of siliciclastic shelf seas.</i> pp. 23-48","BEntID":2986,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: De Batist, M. <i>et al.</i> <i>Geology of siliciclastic shelf seas. Geological Society Special Publication,</i> 117: pp. 23-48","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Jacobs, P.; De Batist, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Jacobs, P.; De Batist, M.","Englishabstract":"In Palaeogene times, the 'Southern Bight' of the North Sea functioned as an intracratonic, shallow-marine, siliciclastic basin and accumulated a few meters of gently dipping sediment packages. A fine-scale seismic-stratigraphical model for the Palaeogene was formulated on the basis of a dense, high-resolution reflection seismic grid. In total 13 major seismic-stratigraphical units were defined, based on geometry and seismic facies characteristics. The seismic stratigraphy has been complemented with the results of four cored wells near the Belgian coast, containing a nearly continuous, 200m thick sediment succession of Eocene age. Facies analysis of these cores suggest that part of these sediments were deposited on a muddy shelf and part in a delta environment. Evidence from relevant onshore outcrops has been used to complete the geological history of the Palaeogene, with special emphasis on the Eocene. A sedimentation model for the Eocene is presented, and relative sea-level changes, regional tectonic events and changes in sediment input are discussed. Genetic interpretation of the various lithological units and the large scale architecture of the ramp-type margin enable evaluation of sequence-stratigraphical concepts, initially defined for a typical shelf-slope-basin section along an Atlantic-type continental margin.","AbstractOtherLang":null,"BibLvlCode":"AMS","StandardTitle":"Sequence stratigraphy and architecture on a ramp-type continental shelf: the Belgian Palaeogene","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2025-07-08 01:30:34.236459","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1996,"MonPub":null,"DateUpdate":"2000-10-13","DateCreate":"2000-08-28","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":2986,"PubliDate":1996,"Pagination":"23-48","XtraPublOfAnaID":null,"ISBN":"1-897799-67-5","Volume":"117","Issue":null,"BRefMon":6486,"BRefMonRR":"<b>De Batist, M.; Jacobs, P. 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