{"refrec":{"BRefID":238419,"RR":"<b>Duperret, A.; Vandycke, S.; Mortimore, R.N.; Genter, A.</b> (2012). How plate tectonics is recorded in chalk deposits along the eastern English Channel in Normandy (France) and Sussex (UK). <i>Tectonophysics 581</i>: 163-181. <a href=\"https://dx.doi.org/10.1016/j.tecto.2012.01.021\" target=\"_blank\">https://dx.doi.org/10.1016/j.tecto.2012.01.021</a>","BEntID":230106,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Tectonophysics 581</i>: 163-181. <a href=\"https://dx.doi.org/10.1016/j.tecto.2012.01.021\" target=\"_blank\">https://dx.doi.org/10.1016/j.tecto.2012.01.021</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Duperret, A.; Vandycke, S.; Mortimore, R.N.; Genter, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Duperret, A. <i>et al.</i>","Englishabstract":"Intra-plate stresses that occurred in the Anglo-Paris Basin and English Channel during Upper Cretaceous and Cenozoic times are a consequence of the convergence between Eurasia and Africa and the opening of the North Atlantic area. This geodynamic re-organisation is recorded on each side of the English Channel, with the emergence of regional structures such as the the Weald-Artois anticline and the reactivation of large-scale strike-slip faults. We analyse the Anglo-Paris Basin Chalk fracture system, on each side of the eastern English Channel, using a set of 1600 meso-scale fractures data collected on coastal chalk cliffs in Normandy (NW France) and Sussex (UK). Meso-scale fracture system is precisely dated using chalk lithostratigraphy correlations within the basin. Moreover, an inversion method is used on fault slip data to evidence a paleostress chronology in the Anglo-Paris Basin. Three main Upper Cretaceous extensive events, characterized by normal faults and jointing are recorded in Normandy and two Cenozoic compressive and extensive events with strike-slip and normal faults appear in Sussex. Paleostress records vary on each part of the eastern English Channel. The meso-scale fracture system is thus used to better define the type of relationship between meso-scale and large-scale brittle deformation in the Chalk during Meso-Cenozoic. A first NE-SW extension is recorded in Normandy in relation with local anticlines structures and related to the Lower Rhine graben opening. A second event is a WNW-ESE extension of local origin in relation with the subsidence axis of the Paris Basin. The third event is a NNE-SSW extension, well marked in Normandy and related to the activation of E-W normal faults in the western approaches of the English Channel. This event is also recorded in Sussex and reactivates locally older fractures in strike-slip. The Oligocene N-S compression/E-W extension related to the Pyrenean tectonics and the last E-W extension relative to the North Sea graben opening are well recorded in Sussex, but not in Normandy. Recent far-field stresses developed in the NW European platform are focused on deep crustal structures like the Artois hills and the Cotentin areas in France. These structures act as a stress barrier by protecting the Normandy Chalk from recent far-field stresses. On the contrary, recent far-field stresses are easily recorded by meso-scale brittle deformation on the folded Chalk in Sussex.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"How plate tectonics is recorded in chalk deposits along the eastern English Channel in Normandy (France) and Sussex (UK)","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":"Chalk; Meso scale fracturing; Paleostress; Lithostratigraphy; TheEastern English Channel; Anglo-Paris basin","OtherDescriptors":null,"Notes":null,"AnaPub":2012,"MonPub":null,"DateUpdate":"2019-06-27","DateCreate":"2014-05-18","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000313761400013","VABBcode":null,"OpenAcc":0,"DOI":"10.1016/j.tecto.2012.01.021"},"refs":null,"anarec":{"AnaID":238419,"PubliDate":2012,"Pagination":"163-181","XtraPublOfAnaID":null,"ISBN":null,"Volume":"581","Issue":null,"BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":44036,"SerRR":"Tectonophysics. ELSEVIER SCIENCE BV: New York; London; Amsterdam.  ISSN 0040-1951; e-ISSN 1879-3266","StandardTitleSer":"Tectonophysics","ISSN":"0040-1951","AbbrevSer":"Tectonophysics","StandardTitleMon":null,"StartPage":163,"Pages":19,"ToPubliDate":null,"BRefBibLvlCode":"S","SerNotes":null},"monrec":null,"serrec":null,"relations":null,"relationsRev":null,"addrec":null,"othpubs":null,"ownerships":null,"authors":[{"AutName":"Duperret","Firstname":null,"Initials":"A.","Affiliation":"Univ Havre, UMR 6294, CNRS, Lab Ondes & MilieuxComplexes, F-76058 Le Havre, France.","Discriminator":null,"CorporateFlag":0,"BEntID":230106,"AutID":180392,"OrderNr":1,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Vandycke","Firstname":"Sara","Initials":"S.","Affiliation":"Université de Mons, Faculté Polytechnique, Géologie Fondamentale et Appliquée","Discriminator":null,"CorporateFlag":0,"BEntID":230106,"AutID":180393,"OrderNr":2,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":"Université de Mons; Faculté Polytechnique; Service de géologie fondamentale et appliquée","ORCID":null,"PersID":37883,"InsID":13967},{"AutName":"Mortimore","Firstname":null,"Initials":"R.N.","Affiliation":"Univ Brighton, Lewes BN7 1BE, Sussex, England.","Discriminator":null,"CorporateFlag":0,"BEntID":230106,"AutID":180394,"OrderNr":3,"DegrID":null,"EditorFlag":0,"CorrespFlag":0,"IllustratorFlag":0,"ReviserFlag":0,"TranslatorFlag":0,"InsAcronym":null,"InsFSN":null,"ORCID":null,"PersID":null,"InsID":null},{"AutName":"Genter","Firstname":null,"Initials":"A.","Affiliation":"Bur Rech Geol & Minieres, F-45060 Orleans, France.","Discriminator":null,"CorporateFlag":0,"BEntID":230106,"AutID":180396,"OrderNr":4,"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":279341,"LibID":36,"BRefID":238419,"EmbargoDate":null,"FullEmbargoDate":null,"PhysMedID":16,"hasOCRd":1,"ShelfLocCode":"279341","RFID":null,"PaidValue":null,"Medium":"Server","Description":null,"Acronym":"VLIZ","Library":"Vlaams Instituut voor de Zee","DutchTerm":"Open Marien Archief","URL":null,"ClassifID":235,"Classification":"Open Marine Archive","ReqLink":null,"ClassifTypID":5,"URLLocation":"https://www.vliz.be/imisdocs/publications/","SubDir":0,"InternalReq":0,"LoggedInReq":0,"Disclaimer":"Disclaimer_OMA","DutchDisclaimer":null,"FileFormat":".pdf","FileDescr":"pdf","InsPub":1,"InsID":36,"FileFormID":6,"LendableFlag":1,"PublicFlag":1,"orderLib":"A","Notes":null,"AccConID":null,"AccessConstraint":null,"LicURL":null}],"litstyles":null,"thespers":null,"arch2discl":null,"SERpubls":[{"PublName":"ELSEVIER SCIENCE BV","City":"New York; London; Amsterdam"}],"MONpubls":null,"pictures":[],"thestermsPath":null,"thestermsASFA":null,"taxtermsASFA":null,"geotermsASFA":null,"collections":[{"Collection":"OMA - Open Marien Archief","ShortName":"OMA"}],"conf":null,"proj":null,"Physdatasets":null,"spcols":{"222":{"SpName":"BMB - Belgische Mariene Bibliografie","SpColID":222,"ParSpColID":null,"TopParID":null,"ShortName":"BMB","URLLocation":null,"LibID":36,"OpenRepoFlag":null,"SpTypID":null,"TopParIDNotWebsite":null,"SpColPath":"BMB"},"221":{"SpName":"OMA - Open Marien Archief","SpColID":221,"ParSpColID":null,"TopParID":null,"ShortName":"OMA","URLLocation":null,"LibID":36,"OpenRepoFlag":1,"SpTypID":null,"TopParIDNotWebsite":null,"SpColPath":"OMA"}},"doi":null,"publs":null,"serparttypes":null,"monauthors":null,"MParts":null,"SParts":null,"hLibs":null,"langs":[{"BEntID":230106,"AbstractFlag":0,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"},{"BEntID":230106,"AbstractFlag":1,"LangID":15,"LangCode":"en","Lang":"English","DutchTerm":"Engels","LangCodeExtended":"eng"}],"urls":[{"URL":"https://dx.doi.org/10.1016/j.tecto.2012.01.021","externalID":"10.1016/j.tecto.2012.01.021","URLTypeCode":"DOI","URLID":34041,"URLTypID":13,"URLType":"DOI","URLPrefix":"http://dx.doi.org/"}],"thesterms":null,"taxterms":null,"geoterms":null,"othterms":null,"asfacodes":null,"asfa2codes":null,"thestermsFRIS":null,"taxtermsFRIS":null,"geotermsFRIS":null,"othtermsFRIS":null,"resmessage":"","complete":1,"sessions":{"newSesName":"Lyssens, Liesbeth, L.","newSesDate":{"date":"2014-05-18 21:53:46.440000","timezone_type":3,"timezone":"Europe/Brussels"},"updSesName":"Bouchti, Zohra, Z.","updSesDate":{"date":"2019-06-27 09:31:49.403000","timezone_type":3,"timezone":"Europe/Brussels"}}}