Abstract
New U–Pb zircon data of a mylonitic greenschist from the Moeche Ophiolite, one of the mafic units involved in the Variscan suture in the Cabo Ortegal Complex (NW of the Iberian Massif), yielded an age of 400 ± 3 Ma. Consequently, this unit can be considered one of the Devonian ophiolites, the most extended group of oceanic units in the Variscan belt. The mafic rocks show transitional compositions between N-MORB and island-arc tholeiites, although Lu–Hf isotope signatures of its zircons clearly indicate contribution from an old continental source. εHf values in the analysed zircons are negative (generally below εHf = −5), and thence, they are not compatible with their generation from a juvenile mantle source. Accordingly, the igneous protoliths were generated in a setting where juvenile mafic magmas interacted with an old continental crust. The Devonian ophiolites from the Variscan suture have been repeatedly interpreted as remnants of the Rheic Ocean. However, the presence of a continental source in the origin of the mafic rocks of the Moeche Ophiolite allows discarding an intraoceanic setting for their generation, at least for the NW Iberian counterparts. The tectonic setting for the Devonian ophiolites of NW Iberia is very likely represented by an ephemeral oceanic basin opened within a continental realm. Herein, the real Rheic Ocean suture could only be located west of the terrane represented by the upper units of the allochthonous complexes. Apparently that suture is not represented in NW Iberia.
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Abati J, Dunning GR, Arenas R, Díaz García F, González Cuadra P, Martínez Catalán JR, Andonaegui P (1999) Early Ordovician orogenic event in Galicia (NW Spain): evidence from U–Pb ages in the uppermost unit of the Ordenes Complex. Earth Planet Sci Lett 165:213–228
Abati J, Castiñeiras P, Arenas R, Fernández-Suárez J, Gómez Barreiro J, Wooden J (2007) Using SHRIMP-RG U–Pb zircon dating to unravel tectonomagmatic events in arc environments. The early Paleozoic arc of NW Iberia revisited. Terra Nova 19:432–439
Abati J, Gerdes A, Fernández-Suárez J, Arenas R, Whitehouse MJ, 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. Geol Soc Am Bull 122:219–235
Albert R, Arenas R, Sánchez Martínez S, Gerdes A (2012) The eclogite facies gneisses of the Cabo Ortegal Complex (NW Iberian Massif): tectonothermal evolution and exhumation model. J Iber Geol 38:389–406
Andonaegui P, Castiñeiras P, González Cuadra P, Arenas R, Sánchez Martínez S, Abati J, Díaz García F, Martínez Catalán JR (2012) The Corredoiras orthogneiss (NW Iberian Massif): geochemistry and geochronology of the Paleozoic magmatic suite developed in a peri-Gondwanan arc. Lithos 128–131:84–99
Arenas R, Gil Ibarguchi JI, González Lodeiro F, Klein E, Martínez Catalán JR, Ortega Gironés E, de Pablo Maciá JG, Peinado M (1986) Tectonostratigraphic units in the complexes with mafic and related rocks of the NW of the Iberian Massif. Hercynica 2:87–110
Arenas R, Rubio Pascual FJ, Díaz García F, Martínez Catalán JR (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. J Metamorph Geol 13:141–164
Arenas R, Abati J, Martínez Catalán JR, Díaz García F, Rubio Pascual FJ (1997) P-T evolution of eclogites from the Agualada Unit (Órdenes Complex, NW Iberian Massif, Spain): implications for crustal subduction. Lithos 40:221–242
Arenas R, Martínez Catalán JR, Sánchez Martínez S, Díaz García F, Abati J, Fernández-Suárez J, Andonaegui P, Gómez-Barreiro J (2007a) Paleozoic ophiolites in the Variscan suture of Galicia (northwest Spain): distribution, characteristics and meaning. In: Hatcher RD Jr, Carlson MP, McBride JH, Martínez Catalán JR (eds) 4-D framework of continental crust. Geological Society of America Memoir, vol, 200, pp 425–444
Arenas R, Martínez Catalán JR, Sánchez Martínez S, Fernández-Suárez J, Andonaegui P, Pearce JA, Corfu F (2007b) The Vila de Cruces Ophiolite: a remnant of the early Rheic Ocean in the Variscan suture of Galicia (Northwest Iberian Massif). J Geol 115:129–148
Arenas R, Sánchez Martínez S, Castiñeiras P, Jeffries TE, 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. J Iber Geol 35:85–125
Ballèvre M, Bosse V, Ducassou C, Pitra P (2009) Palaeozoic history of the Armorican Massif: models for the tectonic evolution of the suture zones. C R Geosci 341:174–201
Ballèvre M, Bosse V, Ducassou C, Paquette JL, Peucat JJ, Pitra P, Poujol M, Ruffet G (2012) Geometry and correlation of the nappe stack in the Ibero-Armorican arc across the Bay of Biscay: a joint French–Spanish project. Part 1: the data. Géol Fr 1:60–61
Beaumont C, Jamieson RA, Butler JP, Warren CJ (2009) Crustal structure: a key constraint on the mechanism of ultra-high-pressure rock exhumation. Earth Planet Sci Lett 287:116–129
Blichert-Toft J, Albarède F (2008) Hafnium isotopes in Jack Hills zircons and the formation of the Hadean crust. Earth Planet Sci Lett 265:686–702
Blichert-Toft J, Puchtel IS (2010) Depleted mantle sources through time: evidence from Lu–Hf and Sm–Nd isotope systematics of Archean komatiites. Earth Planet Sci Lett 297:598–606
Clark AH, Scott DJ, Sandeman HA, Bromley AV, Farrar E (1998) Siegenian generation of the Lizard ophiolite: U–Pb zircon age data for plagiogranite, Porthkerris, Cornwall. J Geol Soc Lond 155:595–598
Corfu F, Hanchar JM, Hoskin PWO, Kinny P (2003) Atlas of zircon textures. In: Hanchar JM, Hoskin PWO (eds) Zircon. Mineralogical Society of America and Geochemical Society, Rev Mineral Geochem 53:468–500
Dallmeyer RD, Martínez Catalán JR, Arenas R, Gil Ibarguchi JI, Gutiérrez Alonso G, Farias P, Aller J, Bastida F (1997) Diachronous Variscan tectonothermal activity in the NW Iberian Massif: evidence from 40Ar/39Ar dating of regional fabrics. Tectonophysics 277:307–337
Díaz García F, Arenas R, Martínez Catalán JR, González del Tánago J, Dunning GR (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 JM, Arenas R (2010) A peri-Gondwanan arc in NW Iberia. II: assessment of the intra-arc tectonothermal evolution through U–Pb SHRIMP dating of mafic dykes. Gondwana Res 17:352–362
Díez Fernández R, Martínez Catalán JR, 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 during the Neoproterozoic and Paleozoic. Gondwana Res 18:385–399
Díez Fernández R, Martínez Catalán JR, Arenas R, Abati J (2011) Tectonic evolution of a continental subduction-exhumation channel: Variscan structure of the basal allochthonous units in NW Spain. Tectonics 30:TC3009
Díez Fernández R, Martínez Catalán JR, Arenas R, Abati J (2012) The onset of the assembly of Pangaea in NW Iberia: constraints on the kinematics of continental subduction. Gondwana Res 22:20–25
Dubińska E, Bylina P, Kozlowski A, Dörr W, Nejbert K (2004) U–Pb dating of serpentinization: hydrothermal zircon from a metasomatic rodingite shell (Sudetic ophiolite, SW Poland). Chem Geol 203:183–203
Fernández-Suárez J, Díaz García F, Jeffries TE, 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
Fernández-Suárez J, Arenas R, Abati J, Martínez Catalán JR, Whitehouse MJ, Jeffries TE (2007) U–Pb chronometry of polymetamorphic high-pressure granulites: an example from the allochthonous terranes of the NW Iberian Variscan belt. In: Hatcher RD Jr, Carlson MP, McBride JH, Martínez Catalán JR (eds) 4-D framework of continental crust. Geological Society of America Memoir, vol 200, pp 469–488
Fuenlabrada JM, Arenas R, Sánchez Martínez S, Díaz García F, Castiñeiras P (2010) A peri-Gondwana arc in NW Iberia. I: isotopic and geochemical constraints on the origin of the arc—a sedimentary approach. Gondwana Res 17:338–351
Fuenlabrada JM, Arenas R, Díez Fernández R, Sánchez Martínez S, Abati J, López Carmona A (2012) Sm-Nd isotope geochemistry and tectonic setting of the metasedimentary rocks from the basal allochthonous units of NW Iberia (Variscan suture, Galicia). Lithos 148:196–208
Gerdes A, Zeh A (2006) Combined U–Pb and Hf isotope LA-(MC)ICP-MS analyses of detrital zircons: comparison with SHRIMP and new constraints for the provenance and age of an Armorican metasediment in Central Germany. Earth Planet Sci Lett 249:47–61
Gerdes A, Zeh A (2009) Zircon formation versus zircon alteration—new insights from combined U–Pb and Lu–Hf in situ LA-ICP-MS analyses, and consequences for the interpretation of Archean zircon from the Limpopo Belt. Chem Geol 261:230–243
Gómez Barreiro J, Martínez Catalán JR, Arenas R, Castiñeiras P, Abati J, Díaz García F, Wijbrans JR (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 RD, 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
Gómez Barreiro J, Martínez Catalán JR, Prior D, Wenk H-R, Vogel S, Díaz García F, Arenas R, Sánchez Martínez S, Lonardelli I (2010) Fabric development in a Middle Devonian intra-oceanic subduction regime: the Careón ophiolite (NW Spain). J Geol 118:163–186
Kryza R, Pin C (2010) The Central-Sudetic ophiolites (SW Poland): petrogenetic issues, geochronology and palaeotectonic implications. Gondwana Res 17:292–305
López-Carmona A, Abati J, Reche J (2010) Petrologic modeling of chloritoid-glaucophane schists from the NW Iberian Massif. Gondwana Res 17:377–391
Ludwig KR (2003) ISOPLOT/Ex, version 3, A Geochronological toolkit for Microsoft Excel. Berkeley Geochronology Center Special Publication, vol 4, 71 pp
Marcos A, Marquínez J, Pérez-Estaún A, Pulgar JA, Bastida F (1984) Nuevas aportaciones al conocimiento de la evolución tectonometamórfica del Complejo de Cabo Ortegal (NW de España). Cuadernos do Lab Xeolóxico Laxe 7:125–137
Martínez Catalán JR, Arenas R, Díaz García F, Rubio Pascual FJ, 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 JR, 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 FJ, Valle Aguado B (2007) Space and time in the tectonic evolution of the northwestern Iberian Massif: implications for the Variscan belt. In: Hatcher RD Jr, Carlson MP, McBride JH, Martínez Catalán JR (eds) 4-D framework of continental crust. Geological Society of America Memoir, vol 200, pp 403–423
Martínez Catalán JR, Arenas R, Abati J, Sánchez Martínez S, Díaz García F, Fernández Suárez J, González Cuadra P, Castiñeiras P, Gómez Barreiro J, Díez Montes A, González Clavijo E, Rubio Pascual FJ, Andonaegui P, Jeffries TE, Alcock JE, Díez Fernández R, López Carmona A (2009) A rootless suture and the loss of the roots of a mountain chain: the Variscan belt of NW Iberia. C.R. Geoscience 341:114–126
Matte Ph (1991) Accretionary history and crustal evolution of the Variscan belt in Western Europe. Tectonophysics 196:309–337
Murphy JB, Gutiérrez-Alonso G (2008) The origin of the Variscan upper allochthons in the Ortegal Complex, northwestern Iberia: Sm–Nd isotopic constraints on the closure of the Rheic Ocean. Can J Earth Sci 4:651–668
Murphy JB, Gutiérrez-Alonso G, Nance RD, Fernández-Suárez J, Keppie JD, Quesada C, Strachan RA, Dostal J (2006) Origin of the Rheic Ocean: rifting along a neoproterozoic suture? Geology 34:325–328
Murphy JB, Cousens BL, Braid JA, Strachan RA, Dostal J, Keppie JD, Nance RD (2011) Highly depleted oceanic lithosphere in the Rheic Ocean: implications for Paleozoic plate reconstructions. Lithos 123:165–175
Nance RD, Gutiérrez-Alonso G, Keppi JD, Linnemann U, Murphy JB, Quesada C, Strachan RA, Woodcock NH (2010) Evolution of the Rheic Ocean. Gondwana Res 17:194–222
Nutman AP, Green DH, Cook CA, Styles MT, Holdsworth RE (2001) SHRIMP U–Pb zircon dating of the exhumation of the Lizard Peridotite and its emplacement over crustal rocks: constraints for tectonic models. J Geol Soc Lond 158:809–820
Ordóñez Casado B, Gebauer D, Schäfer HJ, Gil Ibarguchi JI, Peucat JJ (2001) A single Devonian subduction event for the HP/HT metamorphism of the Cabo Ortegal complex within the Iberian Massif. Tectonophysics 332:359–385
Pearce JA (1996) A users guide to basalt discrimination diagrams. In: Wyman DA (ed) Trace element geochemistry of volcanic rocks: application for massive sulphide exploration. Short Course Notes, Geological Association of Canada, vol 12, pp 79–113
Pereira MF, Chichorro M, Johnston ST, Gutiérrez-Alonso G, Silva JB, Linnemann U, Hofmann M, Drost K (2012) The missing Rheic Ocean magmatic arcs: provenance analyses of Late Paleozoic sedimentary clastic rocks of SW Iberia. Gondwana Res 22:882–891
Peucat JJ, Bernard-Griffiths J, Gil Ibarguchi JI, Dallmeyer RD, Menot RP, Cornichet J, Ponce Iglesias, de León M (1990) Geochemical and geochronological cross section of the deep Variscan crust: the Cabo Ortegal high-pressure nappe (northwestern Spain). Tectonophysics 177:263–292
Pin C, Paquette JL, Santos Zalduegui JF, Gil Ibarguchi JI (2002) Early Devonian supra-subduction zone ophiolite related to incipient collisional processes in the Western Variscan Belt: the Sierra de Careón unit, Órdenes Complex, Galicia. In: Martínez Catalán JR, Hatcher RD Jr, 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 57–71
Pin C, Paquette JL, Ábalos B, Santos JF, Gil Ibarguchi JI (2006) Composite origin of an early Variscan transported suture: Ophiolitic units of the Morais Nappe Complex (north Portugal). Tectonics 25:1–19
Ries AC, Shackleton RM (1971) Catazonal complexes of north-west Spain and north Portugal, remnants of a Hercynian thrust plate. Nat Phys Sci 234:65–68
Rodríguez J, Cosca MA, Gil Ibarguchi JI, Dallmeyer RD (2003) Strain partitioning and preservation of 40Ar/39Ar ages during Variscan exhumation of a subducted crust (Malpica-Tui complex, NW Spain). Lithos 70:111–139
Sánchez Martínez S (2009) Geoquímica y geocronología de las ofiolitas de Galicia. Nova Terra 37:351
Sánchez Martínez S, Jeffries T, Arenas R, Fernández-Suárez J, García-Sánchez R (2006) A pre-Rodinian ophiolite involved in the Variscan suture of Galicia (Cabo Ortegal Complex, NW Spain). J Geol Soc Lond 163:737–740
Sánchez Martínez S, Arenas R, Díaz García F, Martínez Catalán JR, Gómez Barreiro J, Pearce J (2007a) The Careón Ophiolite, NW Spain: supra-subduction zone setting for the youngest Rheic Ocean floor. Geology 35:53–56
Sánchez Martínez S, Arenas R, Andonaegui P, Martínez Catalán JR, Pearce JA (2007b) Geochemistry of two associated ophiolites from the Cabo Ortegal Complex (Variscan belt of northwest Spain). In: Hatcher RD Jr, Carlson MP, McBride JH, Martínez Catalán JR (eds) 4-D framework of continental crust. Geological Society of America Memoir, vol 200, pp 445–467
Sánchez Martínez S, Arenas R, Gerdes A, Castiñeiras P, Potrel A, Fernández-Suárez J (2011) Isotope geochemistry and revised geochronology of the Purrido Ophiolite (Cabo Ortegal Complex, NW Iberian Massif): Devonian magmatism with mixed sources and involved Mesoproterozoic basement. J Geol Soc Lond 168:733–750
Sánchez Martínez S, Gerdes A, Arenas R, Abati J (2012) The Bazar Ophiolite of NW Iberia: a relict of the Iapetus–Tornquist Ocean in the Variscan suture. Terra Nova 24:283–294
Stampfli GM, Borel GD (2002) A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrons. Earth Planet Sci Lett 196:17–33
Taylor SR, McLennan SM (1985) The continental crust: its composition and evolution. Blackwell, Oxford
Vogel DE (1967) Petrology of an eclogite- and pyrigarnite-bearing polymetamorphic rock complex at Cabo Ortegal, NW Spain. Leidse Geol Meded 40:121–213
Warren CJ, Beaumont C, Jamieson RA (2008) Modelling tectonic styles and ultra-high pressure (UHP) rock exhumation during the transition from oceanic subduction to continental collision. Earth Planet Sci Lett 267:129–145
Wedepohl KH (1995) The compositions of the continental crust. Geochim Cosmochim Acta 59:1217–1232
Winchester JA, Pharaoh TC, Verniers J (2002) Palaeozoic amalgamation of Central Europe: an introduction and synthesis of new results from recent geological and geophysical investigations. In: Winchester JA, Pharaoh TC, Verniers J (eds) Palaeozoic amalgamation of Central Europe. Geological Society of London, Special Publication, vol 201, pp 1–18
Wood DA (1980) The application of a Th–Hf–Ta diagram to problems of tectomagmatic classification and to establishing the nature of crustal contamination of basaltic lavas of the British Tertiary Volcanic Province. Earth Planet Sci Lett 50:11–30
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Financial support for this research has been provided by Spanish projects CGL2007-65338-CO2-01 and CGL2012-34618 (Ministerio de Economía y Competitividad). Jürgen Von Raumer and an anonymous reviewer are gratefully acknowledged for insightful reviews of the manuscript.
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Arenas, R., Sánchez Martínez, S., Gerdes, A. et al. Re-interpreting the Devonian ophiolites involved in the Variscan suture: U–Pb and Lu–Hf zircon data of the Moeche Ophiolite (Cabo Ortegal Complex, NW Iberia). Int J Earth Sci (Geol Rundsch) 103, 1385–1402 (2014). https://doi.org/10.1007/s00531-013-0880-x
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DOI: https://doi.org/10.1007/s00531-013-0880-x