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García Lorenzo, Mari Luz ; Abati Gómez, Jacobo ; Orejana García, David ; Castiñeiras García, Pedro ; Crespo Feo, María Elena ; Piña García, Rubén ; García Romero, Emilia ; Granja Bruña, José Luis ; López García, José Ángel ; Fernández Barrenechea, José María ; Arribas Mocoroa, María Eugenia ; Ortega Menor, Lorena ; Pérez Moreno, Elisa María ; Benito Moreno, María Isabel | 2019-06-28texto impreso
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Quijada, I. Emma ; Benito Moreno, María Isabel ; Suárez González, Pablo ; Rodríguez Martínez, Marta ; Campos Soto, Sonia | Elsevier | 2020-10Peritidal carbonate-evaporite successions, since they are developed in the transition between continental and marine realms, provide essential keys for palaeobathymetric and palaeoclimatic interpretations. As a result, several facies models have[...]texto impreso
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Mas Mayoral, José Ramón ; Arribas Mocoroa, María Eugenia ; González Acebrón, Laura ; Quijada, Isabel Emma ; Campos-Soto, S. ; Suárez González, Pablo ; Sacristán Horcajada, Sara ; Arribas Mocoroa, José ; Benito Moreno, María Isabel ; Pérez Garrido, Carlos ; Alonso Millán, Ángela | Springer | 2019-03The early stages of intraplate extensional systems commonly are recorded by deposition of continental sediments. In this context, given appropriate tectonics and eustasy, transgressions can be well recorded in the areas of the basins located clo[...]texto impreso
The microstructure of the rostrum solidum of Jurassic belemnites is compared with that of Sepia cuttlebones, in order to examine possible convergences in their style of growth. For this study, transmitted and polarized light, cathodoluminescence[...]texto impreso
Benito Moreno, María Isabel ; Suárez González, Pablo ; Campos Soto, Sonia ; Rodríguez Martínez, Marta | Springer | 2020The Lower Cretaceous Leza Formation is an essentially carbonate unit deposited at the northernmost active margin of the Cameros Basin (N Spain) under an extensional tectonic regime. This unit is composed of freshwater, marine-influenced, margina[...]texto impreso
Mas Mayoral, José Ramón ; Benito Moreno, María Isabel ; Arribas Mocoroa, José ; Serrano, Ana ; Guimerà Rosso, Joan ; Alonso Millán, Ángela ; Alonso Azcárate, Jacinto | Instituto de Estudios Riojanos (Logroño) | 2002La Cuenca de Cameros, localizada en la parte NO de la Cordillera Ibérica, es una de las cuencas que constituyen el Sistema de Rift Mesozoico Ibérico o Cuenca Ibérica. Se formó en el contexto de la segunda fase de rifting intraplaca que, desde el[...]texto impreso
Quijada, Isabel Emma ; Suárez González, Pablo ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón | SEPM (Society for Sedimentary Geology) | 2013The Lower Cretaceous (Berriasian) Valdeprado Formation (Cameros Basin, northern Spain) contains more than 900 m of laminated carbonates and pseudomorphs after sulfates. Traditionally, many sedimentary packages of different ages and lithologies h[...]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
The last marine Jurassic episode of sedimentation in the Soria area corresponds to the deposition of the Torrecilla en Cameros Fm. during Lower Kimmeridgian. This formation is mainly composed by sandstones, coral reefs and oolites, and is overla[...]texto impreso
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Quijada, Isabel Emma ; Suárez González, Pablo ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón ; Alonso Millán, Ángela | Sociedad Geológica de España | 2010The Late Jurassic-Early Cretaceous Cameros Basin comprises an expanded Tithonian to Early Albian stratigraphic record, mainly made up of fluvial and lacustrine systems, but also containing minor marine incursions. This basin is renowned because [...]
