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The Geology of Madrid Basin in the work of Casiano de Prado (1797-1866)

dc.contributor.authorOrdóñez, Salvador
dc.contributor.authorGarcía del Cura, María Angeles
dc.date.accessioned2015-04-28T08:39:48Z
dc.date.available2015-04-28T08:39:48Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10448
dc.description.abstractAfter Casiano de Prado the infill of Madrid Basin consists of: the "diluvium" or quaternary deposits which surface and thickness was overestimated in his work, and "fresh water tertiary deposits". In the tertiary deposits he distinguished three units: A calcareous upper unit (Colmenar Stone), a gyspsiferous middle unit (Gypsum of Colmenar), and a lower unit that consists of sandstones and conglomerates which outcroppinng in NE and W of the basin, concordant with cretaceous deposits. In his work has been described convoluted and disturbed evaporite deposits, as well as dolostones and siliceous rocks and sepioliteen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherCasiano de Pradoen_US
dc.subject.otherTertiaryen_US
dc.subject.otherMadrid basinen_US
dc.subject.otherHistory of Geologyen_US
dc.titleLa geología de la Cuenca de Madrid en la obra de Casiano de Prado (1797-1866)en_US
dc.titleThe Geology of Madrid Basin in the work of Casiano de Prado (1797-1866)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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