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Browsing by Author Fernández-Suárez, Javier

Showing results 1 to 7 of 7
RightsPreviewIssue DateTitleAuthor(s)Type
openAccessT_2011_30_TC5008.pdf.jpg8-Oct-2011Diachronous post-orogenic magmatism within a developing orocline in Iberia, European VariscidesGutiérrez-Alonso, G.; Fernández-Suárez, Javier; Jeffries, T. E.; Johnston, Stephen T.; Pastor-Galán, Daniel; Murphy, J. Brendan; Franco, M. Piedad; Gonzalo, J. CarlosArtículo
closedAccess15-Aug-2008Genesis and rank distribution of Upper Carboniferous coal basins in the Cantabrian Mountains, Northern SpainColmenero, Juan Ramón; Suárez Ruiz, Isabel; Fernández-Suárez, Javier; Barba, Pedro; Llorens, TeresaArtículo
embargoedAccessGR_2015_28_4_1434.pdf.jpg15-Nov-2014Provenance of the Variscan Upper Allochthon (Cabo Ortegal Complex, NW Iberian Massif)Albert Roper, R.; Arenas, R.; Gerdes, A.; Fernández-Suárez, Javier; Fuenlabrada, J. M.Artículo
openAccess1-Jul-2015Provenance of the Variscan Upper Allochthon (Cabo Ortegal complex, NW Iberian Massif)Albert Roper, R.; Arenas, R.; Gerdes, A.; Sánchez-Martínez, S.; Fernández-Suárez, Javier; Fuenlabrada, J. M.Comunicación de congreso
openAccessJG_2007_115_2_129.pdf.jpgMar-2007The Vila de Cruces Ophiolite: A Remnant of the Early Rheic Ocean in the Variscan Suture of Galicia (Northwest Iberian Massif)Arenas, R.; Martínez Catalán, J. R.; Sánchez Martínez, S.; Fernández-Suárez, Javier; Andonaegui, P.; Pearce, Julian A.; Corfu, FernandoArtículo
closedAccess2007U-Pb depositional age for the upper Barrios Formation (Armorican Quartzite facies) in the Cantabrian zone of Iberia: Implications for stratigraphic correlation and paleogeographyGutiérrez-Alonso, G.; Fernández-Suárez, Javier; Gutiérrez-Marco, J. C.; Corfu, Fernando; Murphy, Brendan; Suárez, MercedesArtículo
openAccess1-Jul-2015Whence come detrital zircons in Siluro-Devonian rocks from Iberia?Fernández-Suárez, Javier; Gutiérrez-Alonso, G.; Pastor-Galán, Daniel; Johnston, Stephen T.; Colmenero, Juan Ramón; Linnemann, U.; Hofmann, M.; Shaw, J.; Hernández, P.Comunicación de congreso