{"refrec":{"BRefID":256855,"RR":"<b>Le Goff, J.; Cerepi, A.; Ghysels, G.; Swennen, R.; Loisy, C.; Heba, G.; El Desouky, H.; Muska, K.</b> (2015). Meter-scale cycles as a proxy for the evolution of the Apulian Carbonate Platform during the late Cretaceous (Llogara Pass, Albania). <i>Facies 61(4)</i>. <a href=\"https://dx.doi.org/10.1007/s10347-015-0448-2\" target=\"_blank\">https://dx.doi.org/10.1007/s10347-015-0448-2</a>","BEntID":248864,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":null,"RefStringPartII":". <i>Facies 61(4)</i>. <a href=\"https://dx.doi.org/10.1007/s10347-015-0448-2\" target=\"_blank\">https://dx.doi.org/10.1007/s10347-015-0448-2</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Le Goff, J.; Cerepi, A.; Ghysels, G.; Swennen, R.; Loisy, C.; Heba, G.; El Desouky, H.; Muska, K.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Le Goff, J. <i>et al.</i>","Englishabstract":"Sedimentological investigations have revealed ten facies in Upper Cretaceous platform carbonates (1220 m thick) at Llogara Pass in southern Albania that can be grouped into four facies associations. These reflect specific environmental conditions, ranging from intertidal to subtidal. The facies form small-scale patterns attesting to high-frequency/low-amplitude cyclicity characteristic of relative sea-level fluctuations. Meter-scale cycles have been classified into six distinct types and characterized on the basis of diagnostic surfaces, diagenetic features, and reservoir properties. A closer look at diagenetic and petrophysical features revealed a drastic porosity reduction at each cycle top (i. e., cycle boundary). This underlines a strong interconnection of facies types and reservoir properties at the cycle scale, thus impacting the whole carbonate succession. The cycle stacking pattern is a reflection of the sedimentary evolution during the late Cretaceous in this southern part of the Apulian Platform. (1) Meter-scale peritidal cycles suggest that the Cenomanian was characterized by stable shallow-water conditions. (2) Thick stromatolitic-dominated cycles typify Turonian deposits. Although the nature of the deposits indicates inner platform conditions, the long-term hiatus documented from Italy (Turonian bauxites) is not evidenced in Llogara. (3) The thin (a few tens of meters) Coniacian-Santonian interval suggests the onset of a significant tectonic control over the sedimentary dynamics, likely accompanied by morphological changes on the Apulian Platform and an emergence of rudist-dominated cycles. (4) Peritidal-subtidal cycles persist during the Campanian, accompanied by a broad development of rudist organisms that evidence significant and repeated relative sea-level rise. These data allow refinement of the general sedimentological evolution during the late Cretaceous on the Apulian Platform.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Meter-scale cycles as a proxy for the evolution of the Apulian Carbonate Platform during the late Cretaceous (Llogara Pass, Albania)","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":"Apulian Platform; Carbonates; Meter-scale cycle; Fischer plots","OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2018-08-31","DateCreate":"2016-05-29","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000362581800003","VABBcode":null,"OpenAcc":0,"DOI":"10.1007/s10347-015-0448-2"},"refs":null,"anarec":{"AnaID":256855,"PubliDate":2015,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"61","Issue":"4","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":123379,"SerRR":"Facies. 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