{"title":"晚新近世穆尔西亚-卡拉斯科盆地扇三角洲斜坡沉积与层序。西班牙)","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":"{\"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}","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}
Fan-delta slope deposits and sequences in the Murcia-Carrasco y Basin (Late Neogene, SE. Spain)
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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