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Autor Quijada, Isabel Emma |
Documentos disponibles escritos por este autor (19)
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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
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
Quijada, Isabel Emma ; Suárez González, Pablo ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón | Sociedad Geológica de España. | 2016Discriminar si el origen de las salmueras en las que precipitaron numerosas sucesiones evaporíticas era marino o continental puede resultar complicado usando exclusivamente criterios sedimentológicos si no contienen fósiles diagnósticos. Éste es[...]texto impreso
Quijada, Isabel Emma ; Suárez González, Pablo ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón | Universidad Complutense de Madrid | 2013The Berriasian Oncala Group of the eastern Cameros Basin is a key element for the paleogeographic reconstruction of NE Iberia during this period of time, due to its intermediate position between the Basque-Cantabrian, southern Iberian, and Pyren[...]texto impreso
Suárez González, Pablo ; Quijada, Isabel Emma ; Mas Mayoral, José Ramón ; Benito Moreno, María Isabel | Sociedad Geológica de España | 2010The Cameros Basin is a rift basin whose sedimentary infill is essentially continental with some episodes of marine influence. The Leza Fm carbonates (Enciso Gr, Barremian-Aptian) correspond to one of these episodes and their depositional environ[...]texto impreso
Suárez González, Pablo ; Quijada, Isabel Emma ; Benito Moreno, María Isabel ; Mas Mayoral, José Ramón | Elsevier | 2014Stromatolite lamination is typically defined as alternation of dark and light laminae. Study of Lower Cretaceous stromatolites fromthe Leza Fm(N Spain) supports this statement, but recognises additional complexities in lamination that have impli[...]