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Anguita, Francisco ; Fernández Caliani, J.C. ; Cordero Tercero, María Guadalupe ; Carrasquilla Ortíz, Sandra ; Anguita, Jorge ; Núñez, Andrés ; Rodríguez, Sergio ; García, Judit | Elsevier | 2006A number of tectonic structures have been located at the Thaumasia Plateau, Daedalia Planum and Aonia Terra, Mars. They include isolated folds with axial traces up to 200 km long, trains of tightly folded structures tens of km long, and thrusts.[...]texto impreso
Fernández Caliani, J.C. ; Crespo Feo, Elena ; Rodas, Magdalena ; Fernández Barrenechea, José María ; Luque del Villar, Francisco Javier | Clay Minerals Society | 2004This paper describes a rare occurrence of nontronite associated with sulfide-bearing felsic metavolcanics, providing evidence of colloidal deposition in open spaces as result of a low-temperature water-rock interaction. Microbotryoidal masses of[...]texto impreso
Rodas, Magdalena ; Luque del Villar, Francisco Javier ; Fernández Barrenechea, José María ; Fernández Caliani, J.C. ; Miras Ruiz, Adolfo ; Fernández Rodríguez, Carlos | Mineralogical Society (Great Britain) | 2000Four distinct associations of graphite have been identified in the low-pressure, high-temperature belt of the Sierra de Aracena (SW Spain). Syngenetic occurrences include: (1) stratiform graphite mineralization within a calc-silicate series; (2)[...]texto impreso
Márquez González, Álvaro ; Fernández Caliani, J.C. ; Anguita, Francisco ; Farelo, Agustín-Felipe ; Anguita, Jorge ; Casa, Miguel Ángel de la | Elsevier Science B.V., Amsterdam | 2004Geological analysis of Mars imagery supports the hypothesis that the planet has been the site of recent (texto impreso
Crespo Feo, Elena ; Luque del Villar, Francisco Javier ; Fernández Rodríguez, Carlos ; Rodas, Magdalena ; Díaz Azpiroz, Manuel ; Fernández Caliani, J.C. ; Fernández Barrenechea, José María | Cambridge University Press | 2004The significance of syngenetic and epigenetic graphite occurrences from the Variscan hightemperature/ low-pressure Aracena Metamorphic Belt is discussed in the framework of the tectonothermal evolution of this southern zone of the Iberian Massif[...]
