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Arribas Mocoroa, María Eugenia ; Arribas Mocoroa, José ; Escavy Fernández, José Ignacio ; Estrada Aliberas, Rita ; Herrero Fernández, Mª Josefa ; Marfil, Rafaela ; Peña, José Andrés de la ; Varas Muriel, María José ; López-Acevedo, Fco. Javier | Universidad Complutense de Madrid | 2015-01-25Se ha llevado a cabo la reconstrucción parcial de la web docente de Petrología Sedimentaria (en la actualidad pendiente de migración) http://www.ucm.es/info/petrosed a la nueva plataforma de Recursos Educativos en Abierto (REA) de la Universidad[...]texto impreso
Arribas Mocoroa, María Eugenia ; Arribas Mocoroa, José ; Peña, José Andrés de la ; Marfil, Rafaela ; Varas Muriel, María José ; López Acevedo, Francisco Javier ; Estrada Aliberas, R. | Universidad Complutense de Madrid | 2011Se presenta por primera vez una página web de carácter docente dedicada a imágenes de microscopía óptica de rocas sedimentarias. Esta página web está vinculada a varias asignaturas de Petrología Sedimentaria que se imparten en el Dpto. de Petrol[...]texto impreso
Caja Rodríguez, Miguel Ángel ; Marfil, Rafaela ; Lago San José, Marceliano ; Salas, Ramón | Sociedad Geológica de España. | 2004A geochemical characterization (major, trace and rare earth element abundances) of the Lower Cretaceous sandstones of the Maestrat Basin has been carried out, in order to discriminate samples from different formations and assess their provenance[...]texto impreso
The Oligocene-Early Miocene As Pontes basin is a non-marine strike-slip basin, filled with small-sized alluvial fan deposits and related coal-bearing lacustr'ine-palustrine successions. The heavy mineral associations were determined in samples c[...]texto impreso
Marfil, Rafaela ; La Iglesia, Á. ; Herrero Fernández, María Josefa ; Scherer, Michael ; Delgado Huertas, Antonio | Wiley | 2015The diagenetic evolution of Permian (Autunian and Saxonian) and Triassic (Buntsandstein) sand-stones and mudrocks have been studied over 1000 m sequence from the Sig€uenza 44-3 drill core inthe Iberian Range, Spain. We compare and contrast the d[...]texto impreso
García Romero, Emilia ; Vegas Salamanca, Juana ; Baldonedo, J.L. ; Marfil, Rafaela | Elsevier | 2005Clay minerals from several volcaniclastic environments including pyroclastic (tuffs), epiclastic (lacustrine, alluvial terraces, marine fan delta) and unconformity-related paleosols in La Palma (Canary Islands) were studied by XRD, SEM, TEM, HRT[...]texto impreso
Caja Rodríguez, Miguel Ángel ; Marfil, Rafaela ; Salas del Mármol, Rafael ; Rossi Nieto, Carlos | Sociedad Geológica de España. | 2001A thick succession of Lower Cretaceous, predominantly continental clastic sediments ("Weald" facies) crop out in the westernmost sub-basins of the Maestrazgo Basin (eastern Iberian Range, Spain). 62 sandstone samples from the Mora, Castellar, an[...]texto impreso
Caja Rodríguez, Miguel Ángel ; Marfil, Rafaela ; Estupiñán Letamendi, Jenny ; Morad, Sadoon ; Mansurbeg, H. ; García, D. ; Amorosi, Alessandro | Sociedad Geológica de España. | 2008The Vøring Basin forms an integrated part of the passive margin off central Norway. Cretaceous sandstones are among the most important hydrocarbon exploration targets in the basin. One of the most significant features of the sandstone reservoirs[...]texto impreso
Caja Rodríguez, Miguel Ángel ; Marfil, Rafaela ; García, D. ; Mansurbeg, H. ; Remacha, E. | Sociedad Geológica de España. | 2006Sandstone turbidites from the Hecho Group in the South-Central Pyrenees are considered exceptional examples for reservoir modelling and outcrop analogous studies. The Hecho Group is divided into four major tectosedimentary units (TSU-2 to TSU-5)[...]texto impreso
Caja Rodríguez, Miguel Ángel ; Salas, Ramón ; Marfil, Rafaela ; Permanyer, A. | Sociedad Geológica de España. | 2008In the Lower Cretaceous sandstones of the Maestrat Basin are present several diagenetic minerals that provide information about their temperature of precipitation. Quartz cement (homogenisation temperatures with a mode of 145ºC), fibrous illite [...]texto impreso
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Herrero Fernández, María Josefa ; Marfil, Rafaela ; Escavy Fernández, José Ignacio ; Al-Aasm, Ihsan ; Scherer, Michael | MDPI | 2020Within the Upper Triassic successions in the Iberian Basin (Spain), the occurrence of both idiomorphic bipyramidal quartz crystals as well as pseudohexagonal aragonite crystals are related to mudstone and evaporite bearing sequences. Bipyramidal[...]texto impreso
Marfil, Rafaela ; Bonhomme, M.G. ; Peña, José Andrés de la ; Penha dos Santos, R. ; Sell, J. | Universidad Complutense de Madrid. Departamento de Estratigraf?a | 1996Las areniscas pérmicas y triásicas de un sondeo de casi mil metros, localizado en Sigüenza (SS-44-3), Cordillera Ibérica, con una composición de sublitoarenitas-grauvacas y arcosas-subarcosas, respectivamente, tienen cementos de ilita formados [...]texto impreso
The Napo Formation of the Cenomaniense age is an importan reservoir-sandstone in the Oriente basin of Ecuador. It displays higher porosity values (average 2 1%) compared to other reservoir in the region. The sandstone are fine to coarse grained [...]texto impreso
Tsige Aga, Meaza ; Caja Rodríguez, Miguel Ángel ; Marfil, Rafaela ; Salas, Ramón ; Martín Crespo, Tomás ; Al-Aasm, Ihsan | Sociedad Geológica de España. | 2004In the western part of the Maestrat Basin (Iberian Range) dolomite and calclte hydrothermal cements fill fractures and "chimney" structures In Tithonian-Berriasian limestones. The timing of fracture cementation is considered in the context of th[...]
