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Sedimentology of the NW part of the Sant Llorenç del Munt fan delta (Eocene, South-Pyrenean foreland basin)

dc.contributor.authorLópez Blanco, M.
dc.contributor.authorMarzo, M.
dc.date.accessioned2017-08-21T11:08:07Z
dc.date.available2017-08-21T11:08:07Z
dc.date.issued1993
dc.identifier.urihttp://hdl.handle.net/10272/14060
dc.description.abstractThe Bartonian-Priabonian Sant Lloreng del Munt fan-delta complex is located at the SE margin of the South-Pyrenean foreland basin. During the deposition of this complex the basin margin was controlled by a series of sinistral strike-slip faults that under transpressive conditions developed some thrusting structures. The fan-delta complex consists of an alternation ofdetrital and carbonate facies. The detrital facies (more than the 9 0 % in volume of the com plex) includ e the deposits of four main facies belts: proximal alluvial fan (conglomerates), distal alluvial fan and fan-delta plain (conglomerates and red sandstones and mudstones), fan-delta front (sandstones and conglomerates) and fan-delta slope (bluegrey offshore marls and "turbiditic" sandstones and conglomerates). The carbonate facies are mainly represented by bioclastic shoals and reefses_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherAlluvial fanes_ES
dc.subject.otherFan deltaes_ES
dc.subject.otherCarbonate platformes_ES
dc.subject.otherEocenees_ES
dc.titleSedimentologia del sector occidental del abanico costerò de Sant Llorenf del Munt (Eoceno, cuenca de antepais surpirenaica)es_ES
dc.titleSedimentology of the NW part of the Sant Llorenç del Munt fan delta (Eocene, South-Pyrenean foreland basin)eng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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