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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
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
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
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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 [...]texto impreso
Suárez González, Pablo ; Quijada, Isabel Emma ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón | Universidad Complutense de Madrid | 2013The Leza Formation is a carbonate unit of the northern Cameros Basin (N Spain) with controversial age, stratigraphic position, and sedimentological interpretation. It was deposited in a series of fault-bounded tectonic depressions along the nort[...]texto impreso
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Quijada, Isabel Emma ; Suárez González, Pablo ; Benito Moreno, María Isabel ; Lugli, Stefano ; Mas Mayoral, José Ramón | Elsevier | 2014Interpreting the origin of carbonate breccias requires a detailed analysis because they may be the result of a wide variety of processes that produce similar features. This is the case of the Lower Cretaceous carbonate breccias of the Cameros Ba[...]texto impreso
Suárez González, Pablo ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón ; Quijada, Isabel Emma ; Campos Soto, Sonia | Sociedad Geológica de España. | 2016Este trabajo aporta nuevos datos cartográficos y sedimentológicos para aclarar la controvertida evolución tectónica extensional de la Cuenca de Cameros (N de España). La geometría actual del borde norte de la cuenca representa la continuación de[...]texto impreso
Suárez González, Pablo ; Arenas Abad, Concha ; Benito Moreno, María Isabel ; Pomar, Luis | Elsevier | 2019-11-01Microbial buildups that predate the Messinian salinity crisis, including one of the few Phanerozoic examples of ‘giant’ microbialites, crop out upon the island of Mallorca (W Mediterranean). Sedimentological and geochemical data from microbialit[...]texto impreso
Campos Soto, Sonia ; Cobos, Alberto ; Caus, Esmeralda ; Benito, María Isabel ; Fernández Labrador, Laura ; Suárez González, Pablo ; Quijada, I. Emma ; Mas, Ramón ; Royo Torres, Rafael ; Alcalá, Alcalá | Elsevier | 2017-11-01The Villar del Arzobispo Formation, cropping out in the western Peñagolosa sub-basin (Late Jurassic, eastern Spain), includes abundant dinosaur tracksites and bones, which occur in diverse mixed siliciclastic and carbonate facies deposited from [...]
