serie NOVA TERRA nº 49

63 for insightful reviews of the manuscript. This paper is a contribution to IGCP Project 497, “ The Rheic Ocean: Origin, evolution and correlatives ” . References Abati, J., Dunning, G.R., Arenas, R., Díaz García, F., González Cuadra, P., Martínez Catalán, J.R., Andonaegui, P., 1999. Early Ordovician orogenic event in Galicia (NW Spain): evidences from U – Pb ages in the uppermost unit of the Órdenes Complex. Earth and Planetary Science Letters 165, 213 – 228. Abati, J., Arenas, R., Martínez Catalán, J.R., Díaz García, F., 2003. Anticlockwise P – T path of granulites from the Monte Castelo Gabbro (Órdenes Complex, NW Spain). Journal of Petrology 44, 305 – 327. Abati, J., Castiñeiras, P., Arenas, R., Fernández-Suárez, J., Gómez-Barreiro, J., Wooden, J., 2007. Using SHRIMP zircon dating to unravel tectonothermal events in arc environments. The early Palaeozoic arc of NW Iberia revisited. Terra Nova 19, 432 – 439. Abati, J., Gerdes, A., Fernández-Suárez, J., Arenas, R., Whitehouse, M.J., Díez Fernández, R., 2010. Magmatism and early-Variscan continental subduction in the northern Gondwana margin recorded in zircons from the basal units of Galicia, NW Spain. Geological Society of America Bulletin 122, 219 – 235. Arenas, R., Rubio Pascual, F.J., Díaz García, F., Martínez Catalán, J.R., 1995. High-pressure microinclusions and development of an inverted metamorphic gradient in the Santiago Schists (Órdenes Complex, NW Iberian Massif, Spain): evidence of subduction and syn-collisional decompression. Journal of Metamorphic Geology 13, 141 – 164. 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 (Northwest Iberian Massif). Journal of Geology 115, 129 – 148. Arenas, R., Sánchez Martínez, S., Castiñeiras, P., Jeffries, T.E., Díez Fernández, R., Andonaegui, P., 2009. The basal tectonic mélange of the Cabo Ortegal Complex (NW Iberian Massif): a key unit in the suture of Pangea. Journal of Iberian Geology 35, 85 – 125. Asiedu, D.K., Dampare, S.B., Asamoah, S.P., Banoeng-Yakubo, B., Osae, S., Nyarko, B.J.B., Many, J., 2004. Geochemistry of Paleoproterozoic metasedimentary rocks from the Birim diamondiferous fi eld, southern Ghana: implications for provenance and crustal evolution at the Archean – Proterozoic boundary. Geochemical Journal 38, 215 – 228. Bathia, M.R., 1983. Plate tectonics and geochemical composition of sandstones. Journal of Geology 91, 611 – 627. Bathia, M.R., Crook, K.A.W., 1986. Trace elements characteristics of graywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology 92, 181 – 193. Casini, L., Oggiano, G., 2008. Late orogenic collapse and thermal doming of the northern Gondwana margin incorporated in the Variscan Chain: a case study from the Ozieri Metamorphic Complex, northern Sardinia, Italy. Gondwana Research 13, 396 – 406. Crook, K.A.W., 1974. Lithogenesis and geotectonics: the signi fi cance of compositional variationsin fl ysch arenites(greywackes).In: Doti,R.H., Shaver,R.H. (Eds.),Modern and Ancient Geosynclinal Sedimentation: Society of Economic Palaeontologists and Mineralogists Special Publication, vol. 19, pp. 304 – 310. DePaolo, D.J., 1981. Neodymium isotopes in the Colorado Front Range and crust – mantle evolution in the Proterozoic. Nature 291, 193 – 196. 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. Journal of Geology 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 Research 17, 352 – 362 (this issue). Elliot, D.H., Fanning, C.M., 2008. Detrital zircons from upper Permian and lower Triassic Victoria Group Sandstones, Shackleton Glacier region, Antarctica: evidence for multiple sources along the Gondwana plate margin. Gondwana Research 13, 259 – 274. 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 granu- lites: an example 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. Fernández-Suarez, J., Corfu, F., Arenas, R., Marcos, A., Martínez Catalán, J.R., Díaz García, F., Abati, J., Fernández, F.J., 2002. U – Pb evidence for a polymetamorphic evolution of the HP – HT units of the NW Iberia Massif. Contributions to Mineralogy and Petrology 143, 236 – 253. Fernández-Suárez, J., Díaz García, F., Jeffries, T.E., Arenas, R., Abati, J., 2003. Constraints on the provenance of the uppermost allochthonous terrane of the NW Iberian Massif: inferences from detrital zircon U – Pb ages. Terra Nova 15, 138 – 144. Gómez Barreiro, J., Martínez Catalán, J.R., Arenas, R., Castiñeiras, P., Abati, J., Díaz García, F., Wijbrans, J.R., 2007. Tectonic evolution of the upper allochthon of the Órdenes complex (northwestern Iberian Massif): structural constraints to a polyorogenic peri-Gondwanan terrane. In: Linneman, U., Nance, R.D., Kraft, P., Zulauf, G. (Eds.), The Evolution of the Rheic Ocean: From Avalonian – Cadomian Active Margin to Alleghenian – Variscan Collision: Geological Society of America Special Paper, vol. 423, pp. 315 – 332. Gutiérrez Alonso, G., Barba, P., Díaz García, F., 2000. Sedimentology and structure of the low grade uppermost unit of the Órdenes Complex at the coastal section. Superposition of structural trends and processes. In: Diaz García, F., González Cuadra,P.,MartínezCatalán,J.R.,Arenas,R.(Eds.),Variscan – AppalachianDynamics: The Building of the Upper Paleozoic Basement. 15th International Conference on Basement Tectonics: A Coruña, Spain, Program and Abstracts Volume, pp. 234 – 235. Hegde, V.S., Chavadi, V.C., 2009. Geochemistry of late Archaean metagreywackes from the Western Dharwar Craton, South India: implications for provenance and nature of the late Archaean crust. Gondwana Research 15, 178 – 187. Herron, M.M., 1988. Geochemical classi fi cation of terrigenous sands and shales from core or log data. Journal of Sedimentary Petrology 58, 820 – 829. Keppie, J.D., Nance, R.D., Murphy, J.B., Dostal, J., Briad, J.A., 2010. The high-pressure Iberian-Czech belt in the Variscan orogen: Extrusion into the upper (Gondwanan) plate? Gondwana Research. 17 (2 – 3), 306 – 316 (this issue). Linneman, U., McNaughton, N.J., Romer, R.L., Gehmlich, M., Drost, K., Tonk, C., 2004. West African provenance for Saxo-Thuringia (Bohemian Massif): did Armorica ever leave pre-Pangean Gondwana? — U/Pb-SHRIMP zircon evidence and the Nd- isotopic record. International Journal of Earth Sciences 93, 683 – 705. Linnemann, U., Romer, R.L., 2002. The Cadomian Orogeny in Saxo-Thuringia, Germany: geochemical and Nd – Sr – Pb isotopic characterization of marginal basins with constraints to geotectonic setting and provenance. Tectonophysics 352, 33 – 64. Martínez Catalán, J.R., Arenas, R., Díaz García, F., Rubio Pascual, F.J., Abati, J., Marquínez, J., 1996. Variscan exhumation of a subducted Paleozoic continental margin: the basal units of the Órdenes Complex, Galicia, NW Spain. Tectonics 15, 106 – 121. Martínez Catalán, J.R., Díaz García, F., Arenas, R., Abati, J., Castiñeiras, P., González Cuadra, P., Gómez Barreiro, J., Rubio Pascual, F., 2002. Thrust and detachment systems in the Órdenes Complex (northwestern Spain): implications for the Variscan – Appalachian geodynamics. In: Martínez Catalán, J.R., Hatcher Jr., R.D., Arenas, R., Díaz García, F. (Eds.), Variscan-Appalachian Dynamics: the building of the Late Paleozoic Basement: Geological Society of America Special Paper, vol. 364, pp. 163 – 182. Martínez Catalán, J.R., Arenas, R., Díaz García, F., González Cuadra, P., Gómez-Barreiro, J., Abati, J., Castiñeiras, P., Fernández-Suárez, J., Sánchez Martínez, S., Andonaegui, P., González Clavijo, E., Díez Montes, A., Rubio Pascual, F.J., Valle Aguado, B., 2007. Space and time in the tectonic evolution of the northwestern Iberian Massif: implications for the 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. 403 – 423. Matte, Ph., 1991. Accretionary history and crustal evolution of the Variscan belt in Western Europe. Tectonophysics 196, 309 – 337. Matte, Ph., Capdevila, R., 1978. Tectonique en grands plis couchés et plissements superposés d´âge hercynien dans la série de Órdenes -Betanzos (Galice Occidentale). Cuadernos del Seminario de Estudios Cerámicos de Sargadelos 27, 193 – 201. McLennan, S.M., Hemming, S.R., 1992. Samarium/neodymium elemental and isotopic systematics in sedimentary rocks. Geochimica et Cosmochimica Acta 56, 887 – 898. McLennan, S.M., Hemming, S.R., McDaniel, D.K., Hanson, G.N., 1993. Geochemical approaches to sedimentation provenance and tectonics: Geological Society of America Special Paper, vol. 284, pp. 21 – 40. Melleton, J., Cocherie, A., Faure, M., Rossi, P., Arenas, R., 2010. Precambrian protoliths and Early Paleozoic magmatism in the French Massif Central: U – Pb data and the North Gondwana connection in the west European Variscan belt. Gondwana Research 17, 13 – 25. Murphy, J.B., Gutiérrez-Alonso, G., Fernández-Suárez, J., Braid, J.A., 2008. Probing crustal and mantle lithosphere origin through Ordovician volcanic rocks along the Iberian passive margin of Gondwana. Tectonophysics 461, 166 – 180. Mutti, E., 1985. Turbidite systems and their relations to depositional sequences. Provenance of arenites. NATO A.S.I. Series 148, 65 – 93. Nakamura, N., 1974. Determination of REE, Ba, Fe, Mg, Na and K in carbonaceous and ordinary chondrites. Geochimica et Cosmochimica Acta 38, 757 – 775. Nance, R.D., Gutiérrez-Alonso, G., Keppie, J.D., Linnemann, U., Murphy, J.B., Quesada, C., Strachan, R.A., Woodcock, N.H., 2010. Evolution of the Rheic Ocean. Gondwana Research 17, 194 – 222 (this issue). Ordoñez Casado, B., Gebauer, D., Schäfer, H.J., Gil Ibarguchi, J.I., Peucat, J.J., 2001. A single Devonian subduction event for the HP/HT metamorphism of the Cabo Ortegal complex within the Iberian Massif. Tectonophysics 332, 359 – 385. Pettijohn, F.H., Potter, P.E., Siever, R., 1972. Sand and Sandstone. Springer-Verlag, New York. 618 p. Pin, C., Paquette, J.L., Santos Zalduegui, J.F., Gil Ibarguchi, J.I., 2002. Early Devonian suprasubduction-zone ophiolite related to incipient collisional processes in the Western Variscan Belt: the Sierra de Careón unit, Órdenes Complex, Galicia. In: Martínez Catalán, J.R., Hatcher Jr., R.D., Arenas, R., Díaz García, F. (Eds.), Variscan – Appalachian Dynamics: The Building of the Late Paleozoic Basement: Geological Society of America Special Paper, vol. 364, pp. 54 – 71. Ranjan, N., Banerjee, D.M., 2009. Central Himalayan crystallines as the primary source for the sandstone – mudstone suites of the Siwalik Group: new geochemical evidence. Gondwana Research 16, 687 – 696. Rodríguez,J.,Cosca,M.A.,GilIbarguchi,J.I.,Dallmeyer, R.D.,2003.Strainpartitioning and preservation of 40 Ar/ 39 Ar ages during Variscan exhumation of a subducted crust (Malpica-Tui complex, NW Spain). Lithos 70, 111 – 139. Roser, B.P., Korsch, R.J., 1985. Plate tectonics and geochemical composition of sandstones: a discussion. Journal of Geology 93, 81 – 84. Roser, B.P., Korsch, R.J., 1986. Determination of tectonic setting of sandstone-mudstone suites using SiO 2 content and K 2 O/Na 2 O ratio. Journal of Geology 94, 635 – 650. Roser, B.P., Korsch, R.J., 1988. Provenance signatures of sandstone – mudstone suites determined using discriminant function analysis of major-element data. Chemical Geology 67, 119 – 139. 350 J.M. Fuenlabrada et al. / Gondwana Research 17 (2010) 338 – 351

RkJQdWJsaXNoZXIy MTQwOQ==