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Autor Ochoa, M. |
Documentos disponibles escritos por este autor (10)
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Arribas Mocoroa, José ; Mas Mayoral, José Ramón ; Ochoa, M. ; Alonso Millán, Ángela | Instituto de Estudios Riojanos (Logroño) | 2002Mediante el estudio petrográfico de los depósitos arenosos pertenecientes a las secuencias deposicionales del relleno de la Cuenca de Cameros, en su margen suroccidental, se han podido definir cuatro petrofacies, que coinciden con las siete secu[...]texto impreso
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Ochoa, M. ; Arribas Mocoroa, José ; Mas Mayoral, José Ramón ; Goldstein, Robert H. | Elsevier | 2007This study provides an example of a high-quality fluvial hydrocarbon reservoir that was completely destroyed by hydrothermal processes. The reservoir unit was deposited in the Cameros Basin, located in the NW sector of the Iberian Chain (Spain).[...]texto impreso
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Buntsandstein deposits generated in a slowly subsiding basin on the western margin of the Iberian Chain are represented by a stratigraphic succession of fluvial deposits less than 100 m thick (conglomerates, sandstones, and shales). Diagenetic p[...]texto impreso
El sondeo surgente de Granátula de Calatrava (activo desde el 25 de julio de 2000 hasta el 16 de enero de 2001) generó un depósito eminentemente arenoso de 36 cm de espesor a 50 m de distancia del pozo. El estudio petrográfico de los materiales [...]texto impreso
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Arribas Mocoroa, José ; Ochoa, M. ; Mas Mayoral, José Ramón ; Arribas Mocoroa, María Eugenia ; González Acebrón, Laura | Universidad Complutense de Madrid | 2007During the most active rifting stages in the northwestern sector of the Iberian Basin (Cameros Basin and Aragonese Branch of the Iberian Range), thick sequences of continental clastic deposits were generated. Sandstone records from Rift cycle 1 [...]texto impreso
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Ochoa, M. ; Arribas Mocoroa, José ; Arribas Mocoroa, María Eugenia ; Mas Mayoral, José Ramón | Geological Society of America | 2007Following the Variscan orogeny, the Iberian plate was affected by an extensional tec-tonic regime from Late Permian to Late Cretaceous time. In the central part of the plate, NW-SE–trending rift basins were created. Two rifting cycles can be ide[...]