La geología de la Cuenca de Madrid en la obra de Casiano de Prado (1797-1866)
| dc.contributor.author | Ordóñez, Salvador | |
| dc.contributor.author | García del Cura, María Angeles | |
| dc.date.accessioned | 2015-04-28T08:39:48Z | |
| dc.date.available | 2015-04-28T08:39:48Z | |
| dc.date.issued | 1997 | |
| dc.description.abstract | After 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 sepiolite | en_US |
| dc.identifier.uri | http://hdl.handle.net/10272/10448 | |
| dc.language.iso | spa | en_US |
| dc.publisher | Sociedad Geológica de España | en_US |
| dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
| dc.rights.accessRights | open access | en_US |
| dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
| dc.subject.other | Casiano de Prado | en_US |
| dc.subject.other | Tertiary | en_US |
| dc.subject.other | Madrid basin | en_US |
| dc.subject.other | History of Geology | en_US |
| dc.title | La geología de la Cuenca de Madrid en la obra de Casiano de Prado (1797-1866) | en_US |
| dc.title | The Geology of Madrid Basin in the work of Casiano de Prado (1797-1866) | eng |
| dc.type | journal article | en_US |
| dspace.entity.type | Publication |
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