{"refrec":{"BRefID":57299,"RR":"<b>Denys, L.; Lebbe, L.; Sliggers, B.C.; Spaink, G.; Van Strijdonck, M.; Verbruggen, C.</b> (1983). Litho- and biostratigraphical study of Quaternary deep marine deposits of the western Belgian coastal plain. <i>Bull. Belg. Ver. Geologie = Bull. Soc. Belg. Geol. 92(2)</i>: 125-154","BEntID":54879,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Bull. Belg. Ver. Geologie = Bull. Soc. Belg. Geol. 92(2)</i>: 125-154","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Denys, L.; Lebbe, L.; Sliggers, B.C.; Spaink, G.; Van Strijdonck, M.; Verbruggen, C.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Denys, L. <i>et al.</i>","Englishabstract":"Elaborate deep borings for hydrogeological purposes in the western part of the Belgian coastal plain revealed the presence of deep marine sediments with different facies. A combined diatom-, mollusc- and pollen investigation procurred many new and interesting data about the diatom flora and the mollusc fauna as well as about the environment and the age of the sediments. The absence of direct reference investigations preventing uniform conclusions at this stage of the investigations. A radio-carbondating and the pollen analysis showed the presence of boreal sediments at the same depth of probably older (Eemian) deposits.","AbstractOtherLang":"Une série de sondages dans le cadre d'une exploration hydrogéologique dans la région de De Panne (plaine maritime belge) a démontré la présence de sédiments marins quaternaires à des profondeurs de plus de 30 m. Une explication pour les grandes différences de facies de ces sédiments ne s'avérait possible que par des recherches paléontologiques détaillées. Ainsi, les examens des diatomées, des mollusques et des pollens ont livré un grand nombre de données nouvelles sur les compositions paléontologiques, le milieu et l'âge des couches. A l'état actuel, l'absence de recherches de références directes n'a pas permis de réunir complètement les résultats des différentes disciplines dans une même conclusion. Néanmoins, une datation C<sub>14</sub> et l'analyse pollinique ont prouvé la présence de sédiments boréals à la même profondeur que des sédiments plus anciens, probablement d'âge Eemien.","BibLvlCode":"AS","StandardTitle":"Litho- and biostratigraphical study of Quaternary deep marine deposits of the western Belgian coastal plain","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":1983,"MonPub":null,"DateUpdate":"2011-07-22","DateCreate":"2004-02-10","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":57299,"PubliDate":1983,"Pagination":"125-154","XtraPublOfAnaID":null,"ISBN":null,"Volume":"92","Issue":"2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45020,"SerRR":"Bulletin van de Belgische Vereniging voor Geologie = Bulletin de la Société Belge de Géologie. 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