{"refrec":{"BRefID":257968,"RR":"Breesch, L.; Swennen, R.; Vincent, B. (2009). Fluid flow reconstruction in hanging and footwall carbonates: compartmentalization by Cenozoic reverse faulting in the Northern Oman Mountains (UAE). Mar. Pet. Geol. 26(1): 113-128. https://dx.doi.org/10.1016/j.marpetgeo.2007.10.004","BEntID":249978,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". Mar. Pet. Geol. 26(1): 113-128. https://dx.doi.org/10.1016/j.marpetgeo.2007.10.004","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Breesch, L.; Swennen, R.; Vincent, B.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Breesch, L.; Swennen, R.; Vincent, B.","Englishabstract":"In this paper. the diagenesis from either side of a major Cenozoic reverse fault in the Northern Oman Mountains is documented. Detailed petrographical and geochemical analysis of calcite-filled fractures in carbonate strata of Late Triassic and Early Cretaceous age in the hanging wall and footwall in Wadi Ghalilah reflect a different diagenetic history. In both hanging wall and footwall most of the fractures are pre-burial, extensional in origin, formed by a crack-seal mechanism, and the calcite vein infill has a host-rock buffered signature. In the hanging wall, the fluid responsible for calcite precipitation of these extensional fractures was a marine fluid at 60 degrees C. These veins predate deep burial and contractional tectonic deformation and consequently do not provide any information about syntectonic fluid flow. Neither do the pre-burial extension fractures in the footwall which are also host-rock buffered. The fractures postdating the tectonic stylolitization in the footwall, by contrast. show evidence of syntectonic migration of saline formation waters at temperatures between 80 and 160 degrees C during contractional deformation. These fluids probably were sourced from the Subsurface via the reverse fault. which acted as a fluid conduit. At the same time, however, this fault functioned as a permeability barrier towards the hanging wall. since no evidence of syntectonic fluid flow is present here. In this way compartmentalization of the hanging wall and footwall block was realized.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Fluid flow reconstruction in hanging and footwall carbonates: compartmentalization by Cenozoic reverse faulting in the Northern Oman Mountains (UAE)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-04-17 01:32:04.522399","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Reverse fault; Veins; Diagenesis; Fluid flown; Compartmentalization","OtherDescriptors":null,"Notes":null,"AnaPub":2009,"MonPub":null,"DateUpdate":"2020-06-19","DateCreate":"2016-05-29","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000261917100006","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.marpetgeo.2007.10.004"},"refs":null,"anarec":{"AnaID":257968,"PubliDate":2009,"Pagination":"113-128","XtraPublOfAnaID":null,"ISBN":null,"Volume":"26","Issue":"1","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43351,"SerRR":"Marine and Petroleum Geology. Elsevier: Guildford. ISSN 0264-8172; e-ISSN 1873-4073","StandardTitleSer":"Marine and Petroleum Geology","ISSN":"0264-8172","AbbrevSer":"Mar. Pet. Geol.","StandardTitleMon":null,"StartPage":113,"Pages":16,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Breesch","Firstname":"Liesbeth","Initials":"L.","Affiliation":"Geologie, K.U. Leuven","Discriminator":null,"CorporateFlag":0,"BEntID":249978,"AutID":228128,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":"Katholieke Universiteit Leuven; Departement Aard- en Omgevingswetenschappen; Afdeling Geologie","ORCID":null,"PersID":33349,"InsID":9768},{"AutName":"Swennen","Firstname":"Rudy","Initials":"R.","Affiliation":"Geologie, K. U. Leuven","Discriminator":null,"CorporateFlag":0,"BEntID":249978,"AutID":139665,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":"Katholieke Universiteit Leuven; Departement Geografie-Geologie","ORCID":"0000-0002-1528-526X","PersID":3679,"InsID":4675},{"AutName":"Vincent","Firstname":null,"Initials":"B.","Affiliation":"Inst Francais Petr, Sedimentol & Stratig Dept, F-92852 Rueil Malmaison, France.","Discriminator":null,"CorporateFlag":0,"BEntID":249978,"AutID":228130,"OrderNr":3,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null}],"mapdetails":null,"datasets":null,"monographs":null,"monparts":null,"serparts":null,"BEntOpen":null,"BEntPrivate":null,"availability":[{"BInstID":346322,"LibID":36,"BRefID":257968,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":null,"ShelfLocCode":"346322","RFID":null,"PaidValue":null,"Medium":"Server","Description":"Interne VLIZ documenten","Acronym":"VLIZ","Library":"Vlaams Instituut voor de Zee","DutchTerm":"Non-open access","URL":null,"ClassifID":228,"Classification":"Non-open access","ReqLink":1,"ClassifTypID":3,"URLLocation":"https://www.vliz.be/imisdocs/publications/","SubDir":1,"InternalReq":1,"LoggedInReq":1,"Disclaimer":"Disclaimer_VLIZ_Intern","DutchDisclaimer":"
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