RT Journal Article
T1 La geología de la Cuenca de Madrid en la obra de Casiano de Prado (1797-1866)
T1 The Geology of Madrid Basin in the work of Casiano de Prado (1797-1866)
A1 Ordóñez, Salvador
A1 García del Cura, María Angeles
AB 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
PB Sociedad Geológica de España
YR 1997
FD 1997
LK http://hdl.handle.net/10272/10448
UL http://hdl.handle.net/10272/10448
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 1 jun 2026