{"refrec":{"BRefID":209600,"RR":"<b>Boës, X.; Hubert-Ferrari, A.; Garcia, D.; Avsar, U.; Damci, E.; Cagatay, N.; Moernaut, J.; De Batist, M.</b> (2009). The Earthquake Sedimentary record of The Lake Hazar along the East Anatolian Fault in Turkey. <i>Geophys. Res. Abstr. 11(EGU2009-13641)</i>","BEntID":201579,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":". <i>Geophys. Res. Abstr. 11(EGU2009-13641)</i>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Boës, X.; Hubert-Ferrari, A.; Garcia, D.; Avsar, U.; Damci, E.; Cagatay, N.; Moernaut, J.; De Batist, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Boës, X. <i>et al.</i>","Englishabstract":"There are a few places in the world where sedimentary records have been studied looking at climate and tectonic interactions. In Turkey, after the destructive Izmit 1999 earthquake, a number of projects have focused on the North Anatolian strike-slip fault in Turkey using lacustrine and marine sedimentary records available in and around the Marmara Sea to further constrain Holocene climatic changes and the occurrence of past major earthquakes. A similar type of study was conducted along the poorly studied the East Anatolian Fault in South-Eastern Turkey using the sedimentary record of the Hazar Lake. The East Anatolian Fault is the conjuguate of the North Anatolian Fault, and a major left-lateral strike-slip fault at the boundary between the Anatolian plate to the North and the Arabian Plate to the South. Like the North Anatolian Fault, it has a long historical record of M=7 earthquakes. The Hazar Lake, in its central part, is considered as an extensional structure in between two major fault segments. The lake, which is 20 km long and 212 m deep, thus contains a unique chronostratigraphic sequence of the deformation occurring along this plate boundary. According to Cetin et al. 2003, the lake record could spend the last 150 ka; this interpretation is confirmed by a new seismic survey and by the study of the first sediment cores collected in the lake in 2007. Our results show that the proximal lake basin is characterized by a continuous sedimentary sequence of ~80 m. The first five meters of lake sediments show series of thin distinct seismo-turbidites preserved between climatically induced sediments. A high resolution radiocarbon age modelling (one radiocarbon date every 200 yr) validate the continuity of the record, making this lake a new valuable high-resolution continental record for the south-east Anatolian region.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"The Earthquake Sedimentary record of The Lake Hazar along the East Anatolian Fault in Turkey","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":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2009,"MonPub":null,"DateUpdate":"2011-11-30","DateCreate":"2011-11-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":1},"refs":null,"anarec":{"AnaID":209600,"PubliDate":2009,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"11","Issue":"EGU2009-13641","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":77248,"SerRR":"Geophysical Research Abstracts. 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