serie NOVA TERRA nº 49

44 Gondwana margin recorded in zircons from the basal units of Galicia, NW Spain. Geol. Soc. Am. Bull. 122, 219 – 235. Albert, R., Arenas, R., Gerdes, A., Sánchez Martínez, S., Fernández-Suárez, J., Fuenlabrada, J.M., 2015. Provenance of the Variscan Upper Allochthon (Cabo Ortegal complex, (NW Iberian massif). Gondwana Res. 28, 1434 – 1448. Andonaegui, P., Castiñeiras, P., González Cuadra, P., Arenas, R., Sánchez Martínez, S., Abati, J., Díaz García, F., Martínez Catalán, J.R., 2012. The corredoiras orthogneiss (NW Iberi- an massif): geochemistry and geochronology of the Paleozoic magmatic suite devel- oped in a peri-gondwanan arc. Lithos 128-131, 84 – 99. Apalategui, O., Pérez-Lorente, F., 1983. Nuevos datos en el borde meridional de la Zona Centroibérica. El dominio Obejo-Valsequillo-Puebla de la Reina. Stud. Geol. Salmanticensia 18, 193 – 200. Araújo, A., Fonseca, P.E., Munhá, J.M., Moita, P., Pedro, J., Ribeiro, A., 2005. The Moura phyllonitic complex: anaccretionarycomplex relatedwith obduction in theSouthern Iberia Variscan suture. Geodin. Acta 18, 375 – 388. Arenas, R., Sánchez Martínez, S., 2015. Variscan ophiolites in NW Iberia: tracking lost Pa- leozoic oceans and the assembly of Pangea. Episodes 38, 315 – 333. Arenas, R., Díez Fernández, R., Sánchez Martínez, S., Gerdes, A., Fernández-Suárez, J., Albert, R., 2014b. Two-stage collision: exploring the birth of Pangea in the Variscan terranes. Gondwana Res. 25, 756 – 763. Arenas, R., Farias, P., Gallastegui, G., Gil Ibarguchi, J.I., González Lodeiro, F., Klein, E., Marquínez, J., Martín Parra, L.M., Martínez Catalán, J.R., Ortega, E., Pablo, Maciá, De, J.G., Peinado, M., Rodríguez Fernández, L.R., 1988. Características geológicas y signi fi cado de los dominios que componen la Zona de Galicia – Trás-os-Montes. Actas del II Congreso Geológico de España, v. Simp., pp. 75 – 84 Arenas, R., Martínez Catalán, J.R., Sánchez Martínez, S., Fernández-Suárez, J., Andonaegui, P., Pearce, J.A., Corfu, F., 2007. The Vila de cruces ophiolite: a remnant of the early Rheic Ocean in the Variscan suture of Galicia (NW Iberian massif). J. Geol. 115, 129 – 148. Arenas, R., Sánchez Martínez, S., Castineiras, P., Jeffries, T.E., Díez Fernández, R., Andonaegui, P., 2009. The basal tectonic melange of the Cabo Ortegal complex (NW Iberian massif): a key unit in the suture of Pangea. J. Iber. Geol. 35, 85 – 125. Arenas, R.,Sánchez Martínez, S., Díez Fernández, R., Gerdes, A., Abati, J., Fernández-Suárez, J., Andonaegui, P., González Cuadra, P., López Carmona, A., Albert, R., Fuenlabrada, J.M., Rubio Pascual, F.J., 2016. Allochthonus terranes involved in the Variscan suture of NW Iberia: a review of their origin and tectonothermal evolution. Earth Sci. Rev. (submitted for publication). Arenas, R., Sánchez Martínez, S., Gerdes, A., Albert, R., Díez Fernández, R., Andonaegui, P., 2014a. Re-interpreting the Devonian ophiolites involvedin the Variscan suture:U – Pb and Lu-Hf zircon data of the Moeche Ophiolite (Cabo Ortegal complex, NW Iberia). Int. J. Earth Sci. 103, 1385 – 1402. Azor, A., 1994. Evolucióntectonometamór fi cadel límite entrelas zonas Centroibérica y de Ossa-Morena (Cordillera Varisca, SO de España) (PhD thesis) Universidad de Granada, Spain (295 pp). Azor, A., González Lodeiro, F., Marcos, A., Simancas, J.F., 1991. Edad y estructura de las rocas de sierra albarrana (SW del macizo Hespérico). Implicaciones regionales. Geogaceta 10, 119 – 124. Azor, A., Lodeiro, F.G., Simancas, J.F., 1994. Tectonic evolution of the boundary between the Central Iberian and the Ossa-Morena zones (Variscan belt, Southwest Spain). Tectonics 13, 45 – 61. Azor, A., Rubatto, D., Simancas, J.F., González Lodeiro, F., Martínez Poyatos, D., Martín Parra, L.M., Matas, J., 2008. Rheic Ocean ophiolitic remnants in southern Iberia questioned by SHRIMP U – Pb zircon ages on the Beja-Acebuches amphibolites. Tectonics 27, TC5006. Ballèvre, M., Martínez Catalán, J.R., López Carmona, A., Abati, J., Díez Fernández, R., Ducassou, C., Pitra, P., Arenas, R., Bosse, V., Castiñeiras, P., Fernández-Suárez, P., Gómez Barreiro, J., Paquette, J.L., Peucat, J.J., Poujol, M., Ruffet, G., Sánchez Martínez, S., 2014. Correlation of the nappe stack in the Ibero-Armorican Arc across the bay of biscay: a joint French – Spanish Project. In: Schulmann, K., Martínez Catalán, J.R., Lardeaux, J.M., Oggiano, G. (Eds.), The Variscan Orogeny: Extent, Timescale and the Formation of the European Crust. Geological Society, London, Special Publications vol. 405, pp. 77 – 113. Booth-Rea, G., Simancas, J.F., Azor, A., Azañón, J.M., González Lodeiro, F., Fonseca, P., 2006. HP-LT Variscan metamorphism in the Cubito-Moura schists (Ossa-Morena zone, southern Iberia). Compt. Rendus Geosci. 338, 1260 – 1267. Borrego, J., Araújo, A., Fonseca, P., 2005. A geotraverse through the south and central sec- tors of the Ossa-Morena Zone in Portugal (Iberian massif). J. Virtual Explor. 19, 1 – 16. Castro, A., 1987. Implicaciones de la Zona Ossa-Morena y dominios equivalentes en el modelo geodinámico de la Cadena Hercínica Europea. Estud. Geol. 43, 249 – 260. Castro, A., Fernández, C., El-Hmidi, H., El-Biad, M., Díaz, M., de la Rosa, J., Stuart, F., 1999. Age constraints to the relationships between magmatism, metamorphism and tecto- nism in the Aracena metamorphic belt, Southern Spain. Int. J. Earth Sci. 88, 26 – 37. Dias da Silva, I., Díez Fernández, R., Díez Montes, A., González Clavijo, E., Foster, D.A., 2015. Magmatic evolution in the N-gondwana margin related to the opening of the Rheic Ocean — evidence from the upper parautochthon of the Galicia - Trás-os-montes zone and from the Central Iberian zone (NW Iberian massif). Int. J. Earth Sci. http:// dx.doi.org/10.1007/s00531-015-1232-9 (in press). Dias da Silva I, Valverde-Vaquero, P., González Clavijo, E., Díez Montes, A., Martínez Catalán, J.R., Schulmann, K., Martínez Catalán, J.R., Lardeaux, J.M., Janousek, V., Oggiano, G., 2014. Structural and stratigraphical signi fi cance of U – Pb ages from the Mora and Saldanha volcanic complexes (NE Portugal, Iberian Variscides). The Variscan Orogeny: Extent, Timescale and the Formation of the European Crust Geo- logical Society of London Special Publication 405, 115 – 135. Díaz García, F., Arenas, R., Martínez Catalán, J.R., González del Tánago, J., Dunning, G.R., 1999. Tectonic evolution of the Careón ophiolite (Northwest Spain): a remnant of oceanic lithosphere in the Variscan Belt. J. Geol. 107, 587 – 605. Díaz García, F., Sánchez Martínez, S., Castiñeiras, P., Fuenlabrada, J.M., Arenas, R., 2010. A peri-Gondwanan arc in NW Iberia. II: assessment of the intra-arc tectonothermal evolution through U – Pb SHRIMP dating of ma fi c dykes. Gondwana Res. 17, 352 – 362. Díaz-Azpiroz, M., Fernández, C., Castro, A., El-Biad, M., 2006. Tectonometamorphic evolu- tion of the Aracena metamorphic belt (SW Spain) resulting from ridge-trench inter- action during Variscan plate convergence. Tectonics 25, TC1001. DíezFernández,R.,Arenas,R.,2015. ThelateDevonianVariscansutureoftheIberianMassif: a correlation of high-pressure belts in NW and SW Iberia. Tectonophysics 654, 96 – 100. Díez Fernández, R., Arenas, R., 2016. Reply to Comment on “ The Late Devonian Variscan suture of the Iberian Massif: a correlation of high-pressure belts in NW and SW Ibe- ria ” . Tectonophysics 670, 155 – 160. Díez Fernández, R., Martínez Catalán, J.R., Arenas, R., Abati, J., 2012a. The onset of the as- sembly ofPangaeainNW Iberia: constraints onthekinematicsof continentalsubduc- tion. Gondwana Res. 22, 20 – 25. Díez Fernández, R., Martínez Catalán, J.R., Arenas, R., Abati, J., Gerdes, A., Fernández- Suárez, J., 2012b. U – Pb detrital zircon analysis of the lower allochthon of NW Iberia: age constraints, provenance and links with the Variscan mobile belt and Gondwanan cratons. J. Geol. Soc. 169, 655 – 665. Díez Fernández, R., Castiñeiras, P., Gómez Barreiro, J., 2012c. Age constraints on lower Pa- leozoic convection system: magmatic events in the NW Iberian Gondwana margin. Gondwana Res. 21, 1066 – 1079. Díez Fernández, R., Foster, D.A., Gómez Barreiro, J., Alonso-García, M., 2013. Rheological control on the tectonic evolution of a continental suture zone: the Variscan example from NW Iberia (Spain). Int. J. Earth Sci. 102, 1305 – 1319. Díez Fernández, R., Martínez Catalán, J.R., Gerdes, A., Abati, J., Arenas, R., Fernández- Suárez, J., 2010. U – Pb ages of detrital zircons from the basal allochthonous units of NW Iberia: provenance and paleoposition on the northern margin of Gondwana dur- ing the Neoproterozoic and Paleozoic. Gondwana Res. 18, 385 – 399. Farias, P., Gallastegui, G., González-Lodeiro, F., Marquínez, J., Martín Parra, L.M., Martínez Catalán, J.R., Pablo Maciá, J.G., de Rodríguez Fernández, L.R., 1987. Aportaciones al conocimiento de la litoestratigrafía y estructura de Galicia central 1. Memórias da Facultade de Ciências, Universidade do Porto, pp. 411 – 431. Faryad, S.W., Kachlík, V., 2013. New evidence of blueschist facies rocks and their geoectonic implication for Variscan suture (s) in the Boheman massif. J. Metamorph. Geol. 31, 63 – 82. Fernández-Suárez, J., Arenas, R., Abati, J., Martínez Catalán, J.R., Whitehouse, M.J., Jeffries, T.E., 2007. U – Pb Chronometry of Polymetamorphic High-Pressure Granulites: An Ex- ample from the Allochthonous Terranes of the NW Iberian Variscan Belt. In: Hatcher Jr., R.D., Carlson, M.P., McBride, J.H., Martínez Catalán, J.R. (Eds.), 4-D Framework of Continental Crust. Geological Society of America Memoir vol. 200, pp. 469 – 488. Franke, W., 2000. The Middle-European Segment of the Variscides: Tectonostratigraphic Units, Terrane Boundaries and Plate Tectonic Evolution. In: Franke, W., Haak, U., Oncken, O., Tanner, D. (Eds.), Orogenic Processes: Quanti fi cation and Modelling in the Variscan Belt. Geological Society London, Special Publication vol. 179, pp. 3 – 61. Franke, W., Engel, W., 1982. Variscan sedimentary basins on the continent and relations with SW England. Proc. Ussher Soc. 5, 259 – 269. Galindo, C., 1989. Petrología y geocronología del complejo plutónico Táliga-Barcarrota (Badajoz) (PhD. thesis) Universidad Complutense de Madrid, Spain (378 pp). Gómez-Barreiro, J., Wijbrans, J.R., Castiñeiras, P., Martínez Catalán, J.R., Arenas, R., Díaz García, F., Abati, J., 2006. 40 Ar/ 39 Ar laserprobe dating of mylonitic fabrics in a polyorogenic terane of NW Iberia. J. Geol. Soc. Lond. 163, 61 – 73. González Cuadra, P., 2007. La Unidad de corredoiras (complejo de Órdenes, Galicia): Evolución estructural y metamór fi ca. Ediciós do Castro, Sada, serie Nova Terra 33 (254 pp). González del Tánago, J., 1995. El núcleo metamór fi co de sierra albarrana y su campo de pegmatitas graníticas asociado, macizo Ibérico, Córdoba, España. Ediciós do Castro, Sada, serie Nova Terra 12 (511 pp). Gutiérrez-Marco, J.C., Sarmiento, G., Rábano, I., 2014. Un olistostroma con cantos y bloques del paleozoico inferior en la Cuenca carbonífera del guadalmellato (Córdoba). Parte II: Bioestratigrafía y a fi nidades paleogeográ fi cas. Rev. Soc. Geol. Esp. 27, 27 – 45. Hatcher Jr., R.D., 1989. Tectonic synthesis of the U.S. Appalachians. In: R.D. Jr., Hatcher, Thomas, W.A., Viele, G.W. (Eds.), The Appalachian-Ouachita orogen in the United States. Geological society Of America, Decade of North American Geology v. F-2, pp. 511 – 531. Hodges, K.V., 2000. Tectonics of the Himalaya and Southern Tibet from two perspectives. Geol. Soc. Am. Bull. 112, 324 – 350. Julivert, M., Fontboté, J.M., Ribeiro, A., Conde, L., 1972. Mapa Tectónico de la Península Ibérica y Baleares E. 1:1.000.000. Instituto Geológico y Minero de España, Madrid. Kroner, U., Romer, R.L., 2013. Two plates — many subduction zones: the Variscan orogeny reconsidered. Gondwana Res. 24, 298 – 329. Kryza, R., Pin, C., 2010. The Central-Sudetic ophiolites (SW Poland): petrogenetic issues, geochronology and palaeotectonic implications. Gondwana Res. 17, 292 – 305. Lardeaux, J.M., Ledru, P., Daniel, I., Duchene, S., 2001. The Variscan French massif central-a new addition to the ultra-high pressure metamorphic ‘ club ’ : exhumation processes and geodynamic consequences. Tectonophysics 332, 143 – 167. Linnemann, U., Herbosch, A., Liégeois, J.P., Pin, C., Gärtner, A., Hofmann, M., 2012. The Cambrian to Devonian odyssey of the Brabant massif within Avalonia: a review with new zircon ages, geochemistry, Sm-Nd isotopes, stratigraphy and palaeogeography. Earth Sci. Rev. 112, 126 – 154. Linnemann, U., Pereira, F., Jeffries, T.E., Drost, K., Gerdes, A., 2008. The cadomian orogeny and the opening of the Rheic Ocean: the diacrony of the geotectonic processes constrained by LA-ICP-MS U – Pb zircon dating (Ossa-Morena and Saxo-Thuringian zones, Iberian and Bohemian massifs). Tectonophysics 461, 21 – 43. López-Guijarro, R., Armendariz, M., Quesada, C., Fernández-Suárez, J., Murphy, J.B., Pin, C., Bellido, F., 2008. Ediacaran – Palaeozoic tectonic evolution of the Ossa-Morena and 142 R. Arenas et al. / Tectonophysics 681 (2016) 135 – 143

RkJQdWJsaXNoZXIy MTQwOQ==