{"refrec":{"BRefID":223644,"RR":"<b>Bless, M.J.M.; Demoulin, A.; Jagt, J.W.M.; Reynders, J.P.H.</b> (1990). The Hautes Fagnes area (NE Belgium) as a Monadnock during the Late Cretaceous. <i>Ann. Soc. géol. Belg. (1968) 113(2)</i>: 75-101","BEntID":215367,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Ann. Soc. Géol. Belg. (1968) 113(2)</i>: 75-101","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Bless, M.J.M.; Demoulin, A.; Jagt, J.W.M.; Reynders, J.P.H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Bless, M.J.M. <i>et al.</i>","Englishabstract":"Morphologically, the Hautes Fagnes area (NE Belgium) is at present a regional high, rising some 100-150 m above the Ardennes plateau, which is slightly inclined to the NW (1°). Recently, a number of residual Late Cretaceous deposits in this area have been sampled in an attempt to reconstruct the gradual Campanian-Maastrichtian transgression onto the area, which acted as a monadnock during this period. Each succession starts with a basal conglomerate, which becomes progressively younger towards the summit of the Hautes Fagnes, indicating the step by step inundation of the area. The deposits have been analysed for bioclast assemblages, fish remains and phosphatised macrofauna, as well as for various microfossil groups, such as forams, ostracodes and sponge spicules. These allow a brief discussion of the paleoenvironment and age of these completely decalcified strata.","AbstractOtherLang":"Morphologiquement, l'aire des Hautes Fagnes (NE de la Belgique) est actuellement un sommet régional qui culmine quelque 100-150m au dessus du plateau de l'Ardenne, faiblement incliné (1°) vers le NW. Récemment, plusieurs dépôts du Crétacé tardif résiduel ont été échantillonnés afin de reconstruire la transgression graduelle Campanienne-Maastrichtienne sur cette aire qui a fonctionné comme un monadnock pendant cette période. Chaque succession commence par un conglomérat de base dont l'âge est progressivement de plus en plus jeune vers le sommet des Hautes Fagnes, indiquant une immersion, étape par étape, de l'aire envisagée. Les dépôts ont été analysés quant à leurs assemblages de bioclastes, de restes de poissons et de macrofaune «phosphatisée» autant que de groupes de microfossiles comme les foraminifères, les ostracodes et les spicules d'éponges. Ceci permet une brève discussion du paléoenvironnement et de l'âge de ces strates complètement décalcifiées.","BibLvlCode":"AS","StandardTitle":"The Hautes Fagnes area (NE Belgium) as a Monadnock during the Late Cretaceous","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-20 01:31:58.417986","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1990,"MonPub":null,"DateUpdate":"2014-09-11","DateCreate":"2013-03-19","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":223644,"PubliDate":1990,"Pagination":"75-101","XtraPublOfAnaID":null,"ISBN":null,"Volume":"113","Issue":"2","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45503,"SerRR":"Annales de la Société géologique de Belgique. Vaillant-Carmanne: Liège.  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