Abstract
The Hercynian Bordères-Louron pluton (20 km2) in the Central Pyrenees intrudes Devonian and Carboniferous metasediments. It shows a concentric zoning and consists of a significant proportion of (quartz) gabbros in its periphery, and of granodiorites, biotite monzogranites and biotite-muscovite monzogranites in its core. AMS study shows that the pluton corresponds to an elongated dome with a N100°E-trending axis. The anisotropy intensity Ppara% is high in the south and in the core of the pluton, whereas it is low in the north. The shape parameter T indicates that the fabric is strongly planar in a large central band oriented NW-SE, whereas it is strongly linear in the western and eastern tips of the pluton. These characteristics suggest that the Bordères-Louron pluton emplaced in two episodes: (1) intrusion of mafic magmas along a N100°E sill parallel to the regional foliation of the host metasediments; and (2) injection of three successive silicic batches (granodiorite, biotite monzogranite, two-micas monzogranite) which pushed aside the early mafic injections. In situ U-Pb dating of zircon grains indicates that the emplacement age of the biotite monzogranite is 309 ± 4 Ma, synchronous with the D 2 dextral transpressive event and close to the ages of the eastern Pyrenean plutons, may be slightly older.
Similar content being viewed by others
References
Auréjac JB, Gleizes G, Diot H, Bouchez JL (2004) Le complexe granitique de Quérigut (Pyrénées, France) revisité par la technique de l’ASM: un pluton syntectonique de la transpression dextre hercynienne. Bull Soc Géol Fr 175:65–82
Barrère P et al (1984) Carte géologique de la France (1/50 000), feuille Arreau. BRGM, Orléans
Borradaile GJ, Henry B (1997) Tectonic applications of magnetic susceptibility and its anisotropy. Earth Sci Rev 42:49–93
Bouchez JL (1997) Granite is never isotropic: an introduction to AMS studies of granitic rocks. In: Bouchez JL, Hutton DHW, Stephens WE (eds) Granite: from segregation of melt to emplacement fabrics. Kluwer, Dordrecht, pp 95–112
Bouchez JL (2000) Anisotropie de susceptibilité magnétique et fabrique des granites. C R Acad Sci Paris 330:1–14
Carreras J, Capella I (1994) Tectonic levels in the Palaezoic basement of the Pyrenees: a review and a new interpretation. J Struct Geol 16:1509–1524
Cocherie A, Baudin T, Autran A, Guerrot C, Fanning MC, Laumonier B (2005) U-Pb zircon (ID-TIMS and SHRIMP) evidence for the early Ordovician intrusion of metagranites in the late Proterozoic Canaveilles Group of the Pyrenees and the Montagne Noire (France): new U-Pb zircon datings. Bull Soc France 176:269–282
Debon F, Enrique P, Autran A (1996) Magmatisme hercynien. In: Barnolas A, Chiron C (eds) Synthèse géologique et géophysique des Pyrénées. Introduction. Géophysique. Cycle hercynien: Edition du Bureau des recherches Géolgiques et Minières et de l’Instituto Tecnologico Geominero de Espana, 729 p
Deloule E, Alexandrov P, Cheilletz A, Laumonier B, Barbey P (2002) In-situ U-Pb zircon ages for Early Ordovician magmatism in the eastern Pyrenees, France: the Canigou orthogneisses. Int J Earth Sci (Geol Rundsch) 91:398–405
Forghani AH (1964) Le massif granitique de Bordères (Hautes-Pyrénées) et son auréole métamorphique. Thèse 3° cycle, Paris
Gleizes G, Nédélec A, Bouchez JL, Autran A, Rochette P (1993) Magnetic susceptibility of the Mont-Louis-Andorra ilmenite-type granite (Pyrenees): a new tool for the petrographic characterisation and the regional maping of zoned granite plutons. J Geophys Res 98:4317–4331
Gleizes G, Leblanc D, Santana V, Olivier P, Bouchez JL (1998a) Sigmoidal structures featuring dextral shear during emplacement of the Hercynian granite complex of Cauterets-Panticosa (Pyrenees). J Struct Geol 20:1229–1245
Gleizes G, Leblanc D, Bouchez JL (1998b) The main phase of the Hercynian orogeny in the Pyrenees is a dextral transpression. In: Holdsworth RE, Strachan RA, Dewey JE (eds) Continental transpressional and transtensional tectonics, vol 135. Geol Soc London, special publications, pp 267–273
Gleizes G, Leblanc D, Olivier P, Bouchez JL (2001) Strain partitioning in a pluton during emplacement in transpressional regime: the example of the Néouvielle granite (Pyrenees). Int J Earth Sci 90:325–340
Guerrot C (1998) Résultats de datation U-Pb par dissolution sur zircons pour le granite de Cauterets, Pyrénées. Rapport inédit, SMN/PEA/ISO 146/98 CG/NB, BRGM. In: Majesté-Menjoulas C, Debon F, Barrère P (eds) Notice explicative, Carte géol. France (1/50 000), feuille Gavarnie (1082). BRGM, Orléans, p 4
Guerrot C (2001) Datation du pluton des Eaux-Chaudes. In: Ternet Y, Majesté-Menjoulas C, Canérot J, Baudin T, Cocherie A, Guerrot C, Rossi P (2004) Notice explicative, Carte géol. France (1/50,000), feuille Laruns-Somport (1069). BRGM, Orléans
Jelinek V (1978) Statistical processing of anisotropy of magnetic susceptibility measured on groups of specimens. Studia Geophys Geod 22:50–62
Lagroix F, Borradaile GJ (2000) Magnetic fabric interpretation complicated by inclusions in mafic silicates. Tectonophysics 325:207–225
Laumonier B, Guitard G, Autran A, Barbey P, Cheilletz A, Baudin T, Cocherie A, Guerrot C (2004) Conséquences de l’absence de socle cadomien sur l’âge et la signification des séries pré-varisques (anté-Ordovicien supérieur) du sud de la France (Pyrénées, Montagne Noire). Bull Soc Géol France 175:643–655
Launeau P, Cruden A, Bouchez JL (1994) Mineral recognition in digital images of rocks: a new approach using multichannel classification. Can Mineral 32:919–933
Lucas Cl (1985) Le grès rouge des Pyrénées. Thèse de doctorat, Toulouse 3
Ludwig KR (2003) User’s manual for a geochronological toolkit for microsoft excel. Berkeley Geochronology Center Special Publication, No 4
Maurel O, Respaut JP, Monié P, Arnaud N, Brunel M (2004) U-Pb emplacement and 40Ar/39Ar cooling ages of the Mont-Louis granite massif (Eastern Pyrenees, France). C R Geosci 336:1091–1098
Olivier Ph, Gleizes G, Paquette JL (2004) Gneiss domes and granite emplacement in an obliquely convergent regime: new interpretation of the Variscan Agly Massif (Eastern Pyrenees, France). In: Whitney DL, Teyssier C, Siddoway CS (eds) Gneiss domes in orogeny, vol 380. Geol Soc Am, pp 229–242
Paquette JL, Gleizes G, Leblanc D, Bouchez JL (1997) Le granite de Bassiès (Pyrénées): un pluton syntectonique d’âge westphalien. Géochronologie U-Pb sur zircons. C R Acad Sci Paris 324:387–392
Roberts MP, Pin C, Clemens JD, Paquette JL (2000) Petrogenesis of mafic to felsic plutonic rock associations: the calc-alkaline Quérigut complex, French Pyrenees. J Petrol 41:809–844
Rochette P (1987) Magnetic susceptibility of the rocks matrix related to magnetic fabric studies. J Struct Geol 9:1015–1020
Romer RL, Soler A (1995) U-Pb age and lead isotopic characterization of Au-bearing skarn related to the Andorra granite (Central Pyrenees, Spain). Mineral Deposita 30:374–383
Soula JC, Debat P, Déramond J, Guchereau JY, Pouget P, Roux L (1986) A dynamic model of the structural evolution of the Hercynian Pyrenees. Tectonophysics 129:29–51
Ternet Y, Barrère P, Debroas EJ (1995) Carte géol. France (1/50 000), feuille Campan (1071). BRGM, Orléans
Vitrac-Michard A, Allègre CJ (1975) 238U-206Pb, 235U-207Pb, systematics on Pyrenean basement. Contrib Mineral Petrol 51:205–212
Acknowledgments
We thank D. Beziat for constructive discussions, R. Peyron and F. de Parseval for thin sections preparation, and C. Cavaré-Hester for her assistance in preparing drawings. This is a contribution of UMR CNRS/UPS 5563 ≪Laboratoire des Mécanismes et Transferts en Géologie≫, Equipe géodynamique.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Gleizes, G., Crevon, G., Asrat, A. et al. Structure, age and mode of emplacement of the Hercynian Bordères-Louron pluton (Central Pyrenees, France). Int J Earth Sci (Geol Rundsch) 95, 1039–1052 (2006). https://doi.org/10.1007/s00531-006-0088-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00531-006-0088-4