La geología de la Cuenca de Madrid en la obra de Casiano de Prado (1797-1866)

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1997

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Sociedad Geológica de España
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https://hdl.handle.net/20.500.14352/120897

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Ordóñez Delgado, S. y García del Cura, M. A. (1997) «La geología de la Cuenca de Madrid en la obra de Casiano de Prado ( 1797-1866)», Geogaceta, 23, pp. 107-109.

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.

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Geología

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2506.01 Geología Regional, 5506.09 Historia de la Geología

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