{"title":"Fan-delta slope deposits and sequences in the Murcia-Carrasco y Basin (Late Neogene, SE. Spain)","authors":"C. Dabrio, M. Polo","doi":"10.5209/REV_CGIB.1991.V15.2620","DOIUrl":null,"url":null,"abstract":"Tortonian sedimeratation isa dio Betics records a major tectonie evont, tite Iargost orogenic deformation of dio cordillera, suporimposed on tite largorscale, titird-orderTB 3.2 cycle ofeustatie sea-lovelcitange. A ftrst interprotation of the Sequonce Stratigraplty of tite Murcia-Carrascoy basin is prosented. Uplift of positivo reliefs aronrad tite basin favaured tite depositiora of titick successions of conglomoratos evidoncing c?mnibalism. Facies associations witness doposition on tite steep siopo of a basin, fod by mauntain rivors titat supplied coarso sedimesats to tite basin. Tite resulting fara delta is comparable in many respocts to titoso describod isa fjords, and a dopositional model is presonted.","PeriodicalId":110220,"journal":{"name":"Journal of iberian geology: an international publication of earth sciences","volume":"179 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of iberian geology: an international publication of earth sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.5209/REV_CGIB.1991.V15.2620","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 5
Abstract
Tortonian sedimeratation isa dio Betics records a major tectonie evont, tite Iargost orogenic deformation of dio cordillera, suporimposed on tite largorscale, titird-orderTB 3.2 cycle ofeustatie sea-lovelcitange. A ftrst interprotation of the Sequonce Stratigraplty of tite Murcia-Carrascoy basin is prosented. Uplift of positivo reliefs aronrad tite basin favaured tite depositiora of titick successions of conglomoratos evidoncing c?mnibalism. Facies associations witness doposition on tite steep siopo of a basin, fod by mauntain rivors titat supplied coarso sedimesats to tite basin. Tite resulting fara delta is comparable in many respocts to titoso describod isa fjords, and a dopositional model is presonted.
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