Información del autor
Documentos disponibles escritos por este autor (8)
Añadir el resultado a su cesta Hacer una sugerencia Refinar búsqueda
texto impreso
Arribas Mocoroa, José ; Díaz Molina, Margarita ; Tortosa, A. | Universidad Complutense de Madrid. Departamento de Estratigrafía | 1996Las sucesiones estratigráficas del Mioceno inferior en la cuenca de Loranca (sistemas deposicionales de Tórtola, Villalba de la Sierra y Valdeganga) presentan depósitos interestratificados de playa-lake y de ríos meandriformes. En este trabajo s[...]texto impreso
texto impreso
Díaz Molina, Margarita ; Kälin, Otto ; Benito Moreno, María Isabel ; López Martínez, Nieves ; Vicens, Enric | Elsevier | 2007-07-15The Late Cretaceous Aren Fm exposed north of Bastus in the Tremp Basin (south-central Pyrenees) preserves an excellent record of dinosaur eggs laid in a marine littoral setting. Different from other cases reported in literature, at the Bastus si[...]texto impreso
Sanz , J.L. ; Moratalla, J.J. ; Díaz Molina, Margarita ; López Martínez, Nieves ; Kälin, Otto ; Vianey-Liaud, M. | Nature Publishing Group | 2002-08-31texto impreso
texto impreso
Díaz Molina, Margarita ; Arribas Mocoroa, José ; Gómez Fernández, Juan José ; Tortosa, A. | Geological Society of London | 1995The reconstruction of meander belts was approached by detailed geological mapping, the interpretation of exposed sandstone bodies and the application of sedimentological concepts. The single reconstructed meander belts were integrated, consideri[...]texto impreso
Díez Canseco, Davinia ; Buatois, Luis A. ; Mángano, M. Gabriela ; Díaz Molina, Margarita ; Benito Moreno, María Isabel | The Paleontological Society. | 2016The Upper Cretaceous “redbeds” of the lower Tremp Formation (South-Central Pyrenees, Spain) contains an ichnofauna consisting of Taenidium barretti, Taenidium bowni, Loloichnus isp., Arenicolites isp., Planolites isp., and Palaeophycus isp. This[...]texto impreso
Arribas Mocoroa, María Eugenia ; Doval, Mercedes ; Díaz Molina, Margarita | Sociedad Geológica de España | 1995The study of the clay minerals in the Upper Unit (Upper Oligocene - Lower Miocene) in Loranca Basin shows a change from the bottom (subunit 1) to the top (subunit 2). Subunit 1 is characterized by the clay mineral association 1, when the great p[...]
