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Clay authigenesis mostly concerns: (a) the formation of clays by direct precipitation from solution, called “neoformation” and (b) development of clays by transformation of precursor minerals. Precipitation from solution implies that a new miner[...]texto impreso
Pozo, M. ; Casas, J. ; Medina, J.A. ; Calvo Sorando, José Pedro ; Silva Barroso, Pablo Gabriel | Consejo Superior de Investigaciones Científicas, Museo Nacional de Ciencias Naturales | 2006En la zona de canteras de Valdeinfierno, en el sector de Batallones-Malcovadeso, parte centro-meridional de la Cuenca de Madrid, se ha reconocido una serie de depósitos carbonáticos que presentan geometría dómica y estructura interna columnar. D[...]texto impreso
Pozo, M. ; Sanz Rubio, E. ; Rodríguez Aranda, Juan Pablo ; Casas Sainz de Aja, J. ; Calvo Sorando, José Pedro ; Cañaveras, Juan Carlos | Sociedad Geológica de España. | 2000Sedimentary magnesite is largely present in the Miocene evaporite formations (Lower and Intermediate units) of the Calatayud Basin (NE Spain). Magnesite deposits are forming part of sedimentary sequences corresponding to hypersaline and moderate[...]texto impreso
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Pozo, M. ; Calvo Sorando, José Pedro ; Bustillo Revuelta, Manuel ; Kilias, Stephanos P. ; Stamatakis, Michael G. | Sociedad Geológica de España. | 2004The Rubian sparry magnesite (Galicia, NW Spain) is hosted in Lower Cambrian carbonate rocks (Caliza de Cándana Fm.) included in a strongly deformed and faulted thick succession of siliciclastic and carbonate rocks. The magnesite shows massive an[...]texto impreso
Kilias, Stephanos P. ; Pozo, M. ; Bustillo Revuelta, Manuel ; Stamatakis, Michael G. ; Calvo Sorando, José Pedro | Springer Science Business Media | 2006The Rubian magnesite deposit (West Asturian—Leonese Zone, Iberian Variscan belt) is hosted by a 100-m-thick folded and metamorphosed Lower Cambrian carbonate/siliciclastic metasedimentary sequence—the Cándana Limestone Formation. It comprises up[...]texto impreso
Calvo Sorando, José Pedro ; Pozo, M. ; Silva Barroso, Pablo Gabriel ; Morales, Jorge | Blackwell Publishing Ltd | 2013Fossil mammal sites of late Miocene age (ca 9 Ma) occur in hourglassshaped, non-interconnected cavities up to 15 m deep, hosted in mudstone (mostly sepiolite), chert and carbonate bedrock in Cerro de los Batallones. This paper provides a model f[...]texto impreso
Pozo, M. ; Calvo Sorando, José Pedro ; Scopelliti, G. ; González Acebrón, Laura | Elsevier B.V. | 2016A number of carbonate mounds composed of indurate, strongly folded and/or brecciated calcite and dolomite beds occur interstratified in Cenozoic sedimentary sequences from the Las Minas Basin. Part of the fabric of the rock forming the carbonate[...]
