{"refrec":{"BRefID":338001,"RR":"<b>Munsterman, D.K.; Deckers, J.</b> (2020). The Oligocene/Miocene boundary in the ON-Mol-1 and Weelde boreholes along the southern margin of the North Sea Basin, Belgium. <i>Geol. Belg. 23(3-4)</i>: 127-135. <a href=\"https://hdl.handle.net/10.20341/gb.2020.007\" target=\"_blank\">https://hdl.handle.net/10.20341/gb.2020.007</a>","BEntID":334625,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Geol. Belg. 23(3-4)</i>: 127-135. <a href=\"https://hdl.handle.net/10.20341/gb.2020.007\" target=\"_blank\">https://hdl.handle.net/10.20341/gb.2020.007</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Munsterman, D.K.; Deckers, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Munsterman, D.K.; Deckers, J.","Englishabstract":"Based on palynologic interpretations, the Oligocene/Miocene boundary was identified in the cored samples of the ON-Mol-1 and Weelde boreholes in the southern North Sea Basin. In both boreholes, the presume:I location of the Oligocene/Miocene boundary is marked by a thin gravel bed, which testifies of a hiatus, within a continuation of shelly, dark green to black fine glauconitic sands. In the Weelde borehole, the hiatus is relatively short as the dinocysts under- and overlying the gravel bed suggest a late(st) Chattian and early Aquitanian age. This study thereby for the first time indicates the presence of Aquitanian strata in the area. In the ON-Mol-1 borehole, located south of the Weelde borehole, the hiatus is longer as dinocysts under- and overlying the gravel bed suggest an early Chattian and late Aquitanian age. The wider ranges of the hiatus might be the result of the combination of erosion/non-deposition of late Chattian strata and the gradual transgression of the southern North Sea Basin from north to south after the Oligocene/Miocene sea-level fall. The sampled interval around the Oligocene/Miocene boundary contains a lot of reworked Paleogene (including irregular upper Oligocene species occurrences) and Mesozoic taxa, which explains why the Miocene strata in the ON-Mol-1 and Weelde boreholes were dated as Chattian by previous studies.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The Oligocene/Miocene boundary in the ON-Mol-1 and Weelde boreholes along the southern margin of the North Sea Basin, Belgium","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-25 01:33:19.255792","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Palynology, dinoflagellate cysts, age assessment, facies, reworking, gravel beds, Campine Block, Savian phase","OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2021-05-29","DateCreate":"2021-05-17","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000607869400008","VABBcode":null,"OpenAcc":1,"Handle":"10.20341/gb.2020.007"},"refs":null,"anarec":{"AnaID":338001,"PubliDate":2020,"Pagination":"127-135","XtraPublOfAnaID":null,"ISBN":null,"Volume":"23","Issue":"3-4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":45707,"SerRR":"Geologica Belgica. 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