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Rojo-Pérez, Esther ; Arenas Martín, Ricardo ; Fuenlabrada Pérez, José Manuel ; Sánchez Martínez, Sonia ; Martín Parra, Luis Miguel ; Matas, Jerónimo ; Pieren Pidal, Agustín Pedro ; Díez Fernández, Rubén | Elsevier | 2019-05In the Iberian Massif, westernmost sector of the Variscan Orogen, the nature of the boundary between the Central Iberian Zone and the Ossa Morena Complex has been largely discussed. Peri-Gondwanan Ediacaran series similar in age (c. 565?Ma) but [...]texto impreso
Díez Fernández, Rubén ; Arenas Martín, Ricardo ; Pereira, M. Francisco ; Sánchez Martínez, Sonia ; Albert Roper, Richard ; Martín Parra, Luis-Miguel ; Rubio Pascual, Francisco-J. ; Matas, Jerónimo | Elsevier | 2016-11An integrated interpretation of the late Paleozoic structural and geochronological record of the Iberian Massif is presented and discussed under the perspective of a Gondwana-Laurussia collision giving way to the Variscan orogen. Compressional a[...]texto impreso
Tejero López, Rosa ; Carbonell, R. ; Ayarza Arribas, Puy ; Azor Pérez, Antonio ; García Lobón, J.L. ; González Cuadra, Pablo ; González Lodeiro, Francisco ; Jabaloy Sánchez, Antonio ; Mansilla Plaza, Luis ; Martín Parra, Luis Miguel ; Martínez Poyatos, D. ; Matas, Jerónimo ; Palomeras, Inmaculada ; Pérez Estaún, A. ; Simancas Cabrera, José Fernando | Sociedad Geológica de España. | 2008The 250 km long, vertical incidence seismic reflection profile ALCUDIA was acquired in spring 2007. It samples the Variscan Central Iberian Zone from Toledo to Fuenteovejuna. Its main goal was to continue the structure obtained for the crust and[...]texto impreso
Arenas Martín, Ricardo ; Fernández Suárez, Javier ; Montero, Pilar ; Díez Fernández, Rubén ; Andonaegui Moreno, Pilar ; Sánchez Martínez, Sonia ; Albert Roper, Richard ; Fuenlabrada Pérez, José Manuel ; Matas, Jerónimo ; Martín Parra, Luis Miguel ; Rubio Pascual, Francisco J. ; Jiménez Díaz, Alberto ; Pereira, M. Francisco | Elsevier | 2018-07In the Ossa Morena Domain of SW Iberia, the Calzadilla Ophiolite is formed by an ensemble of ultramafic and mafic rocks that seem to represent a fragment of an oceanic Moho transition zone. The ophiolite consists of a main sheet with a minimum t[...]texto impreso
Arenas Martín, Ricardo ; Díez Fernández, Rubén ; Rubio Pascual, Francisco J. ; Sánchez Martínez, Sonia ; Martín Parra, Luis Miguel ; Matas, Jerónimo ; González del Tánago y del Río, José ; Jiménez Díaz, Alberto ; Fuenlabrada, José M. ; Andonaegui Moreno, Pilar ; Garcia Casco, Antonio | Elsevier | 2016-06Correlation of a group of allochthonous terranes (referred to as basal, ophiolitic and upper units) exposed in theNW and SW of the Iberian Massif, is used to propose a new geotectonic zone in the southern branch of theVariscan Orogen: the Galici[...]
