Skip to main content
Log in

The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights

  • Original Paper
  • Published:
International Journal of Earth Sciences Aims and scope Submit manuscript

Abstract

The Léon Domain in the NW part of the French Massif Armoricain is a stack of synmetamorphic nappes displaced from south to north in ductile conditions. From bottom to top, an orthogneissic basement is overthrusted successively by (1) a Lower Nappe of gneiss including mafic eclogites, (2) an Intermediate Nappe of biotite–garnet–staurolite micaschists with mafic blocks, and (3) an upper nappe made up of Neoproterozoic phyllites covered by unmetamorphosed Paleozoic sedimentary series. This microstructural study documents a polyphase evolution with firstly a top-to-the-N shearing, secondly followed by upright folding of the stack of nappes coeval with migmatization, and lastly, a dextral wrenching along the North Armorican Shear Zone associated with emplacement of synkinematic plutons. New U–Th/Pb chemical dating of monazites from biotite–garnet–staurolite micaschists, migmatites, and granitoids argue for 340–335 Ma, 335–327 Ma, and about 320 Ma ages for synthrusting metamorphism, anatexis, and wrenching, respectively. A metagabbro from Le Conquet yields a zircon LA-ICP-MS age of 478 ± 4 Ma, which corresponds to magma emplacement time. The Léon Domain is interpreted as a microcontinent separated from Armorica by the Le Conquet-Penzé suture to the south and east, and from Laurussia by the Rheic suture to the north. A possible correlation with the Mid-German Crystalline Rise of Central Europe is discussed.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11
Fig. 12
Fig. 13
Fig. 14
Fig. 15
Fig. 16
Fig. 17

Similar content being viewed by others

References

  • Altherr R, Henes-Klaiber U, Hegner E, Satir M, Langer C (1999) Plutonism in the Variscan Odenwald (germany): from subduction to collision. Int J Earth Sci 88:422–443. doi:10.1007/s005310050276

    Article  Google Scholar 

  • Balé P, Brun JP (1986) Les complexes métamorphiques du Léon (NW Bretagne): un segment du domaine éo-hercynien sud armoricain translaté au Dévonien Bull. Soc Geol Fr 2:471–477

    Google Scholar 

  • Ballèvre M, Marchand J, Godard G, Goujou JC, Wyns R (1994) Eo-Hercynian events in the Massif Armoricain. In: Keppie JD (ed) Pre-Mesozoic geology of France and related areas. Springer, Berlin, pp 183–194

    Google Scholar 

  • Be Mezème E, Faure M, Cocherie A, Chen Y (2005) In situ chemical dating of tectonothermal events in the French Variscan Belt. Terra Nova 17:420–426. doi:10.1111/j.1365-3121.2005.00628.x

    Article  Google Scholar 

  • Bois C, Cazes M, Choukroune P, Garrel O, Hirn A, Le Gall B et al (1994) Seismic reflection images of the Pre-Mesozoic crust in France and adjacent areas. In: Keppie JD (ed) Pre-Mezozoic geology of France and related areas. Springer, Berlin, pp 3–48

    Google Scholar 

  • Braun I, Montel JM, Nicollet C (1998) Electron microprobe dating of monazite from high-grade gneisses and pegmatites of Kerala Khondalite Belt, Southern India. Chem Geol 146:65–85. doi:10.1016/S0009-2541(98)00005-9

    Article  Google Scholar 

  • Cabanis B, Godard G (1987) Les éclogites du pays de Léon (nord-Ouest du Massif armoricain): étude pétrologique et géochimique; implications géodynamiques. Bull Soc Geol Fr 6:1133–1142

    Google Scholar 

  • Cabanis B, Peucat J, Michot J, Deutsch S (1979) Remise en cause de l’existence d’un socle orthogneissique antécambrien dans le pays de Léon (domaine Nord-armoricain); étude géochronologique par les méthodes Rb/Sr et U/Pb des orthogneiss de Tréglonou et de Plouvenez-Lochrist. Bull BRGM 4:357–364

    Google Scholar 

  • Chauris L, Hallégouet B (1989) Carte géologique de France 1/50.000 et notice explicative, feuille Le Conquet, BRGM, Orléans, 69 pp

  • Chauris L, Marcoux E, Le Goff E, Thiéblement D, Carn A (1998) Carte géologique de France 1/50.000 et notice explicative, feuille Saint-Pol de Léon, BRGM, Orléans, 167 pp

  • Cocherie A, Albarède F (2001) An improved U–Th–Pb age calculation for electron microprobe dating of monazite. Geochim Cosmochim Acta 65:4509–4522. doi:10.1016/S0016-7037(01)00753-0

    Article  Google Scholar 

  • Cocherie A, Legendre O (2007) Potential minerals for determining U–Th–Pb chemical age using electron microprobe. Lithos 93(3/4):288–309. doi:10.1016/j.lithos.2006.03.069

    Article  Google Scholar 

  • Cocherie A, Robert M (2007) Direct measurement of lead isotope ratios in low concentration environmental samples by MC-ICP-MS and multi-ion counting. Chem Geol 243:90–104. doi:10.1016/j.chemgeo.2007.05.011

    Article  Google Scholar 

  • Cocherie A, Robert M (2008) Laser ablation coupled with ICP-MS applied to U–Pb zircon geochronology: a review of recent advances. Gondwana Res Special Issue (in press)

  • Cocherie A, Legendre O, Peucat JJ, Kouamelan AN (1998) Geochronology of polygenetic monazites constrained by in situ electron microprobe U–Th–total lead determination: implications for lead behaviour in monazite. Geochim Cosmochim Acta 62:2475–2497. doi:10.1016/S0016-7037(98)00171-9

    Article  Google Scholar 

  • Cocherie A, Be Mezème E, Legendre O, Fanning CM, Faure M, Rossi P (2005) Electron-microprobe dating as a tool for determining the closure of Th–U–Pb systems in migmatitic monazites. Am Mineral 90:607–618. doi:10.2138/am.2005.1303

    Article  Google Scholar 

  • Cocherie A, Fanning CM, Jezéquel P, Robert M (2007) LA-MC-ICPMS applied to in situ U-Pb dating of 2 Ma zircons using a multi-ion counting system. Electron microscopy and microanalysis conference. In: Mineralogical Society of Poland—special papers 30. Mineralogical Society of Poland, Krakow, pp 61–63

  • Cogné J (1974) Le Massif Armoricain. In: Debelmas J (ed) Géologie de la France. Doin, Paris, pp 105–161

    Google Scholar 

  • Deutsch S, Chauris L (1965) Age de quelques formations cristallophylliennes et granitiques du Pays de Léon (Finistère). C R Acad Sci Paris 260:615–617

    Google Scholar 

  • Edel JB, Weber K (2004) Cadomian terranes, wrench faulting and thrusting in the central Europe Variscides: geophysical and geological evidence. Int J Earth Sci 84:412–432

    Google Scholar 

  • Faure M, Bé Mézème E, Duguet M, Cartier C, Talbot J (2005) Paleozoic tectonic evolution of Medio-europa from the example of the French Massif Central and Massif Armoricain. In: Carosi R, Dias R, Iacopini D, Rosenbaum G (eds) The southern Variscan belt. J Virt Explor, electronic edition, ISSN 1441–8142, vol 19, paper 5

  • Franke W (2000) The Mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution. In: Franke W, Haak V, Oncken O, Tanner D (eds) Quantification and modelling in the Variscan Belt (Geological Society of London special publication 179). Geological Society, London, pp 21–34

    Google Scholar 

  • Goré B, Le Corre C (1987) Cinématique hercynienne du cisaillement nord-armoricain à la bordure du granite syntectonique de St Renan-Kerstaint (Finistère). Bull Soc Geol Fr 5:811–819

    Google Scholar 

  • Holder MT, Leveridge BE (1986) Correlation of the Rhenohercynian Variscides. J Geol Soc Lond 143:141–147. doi:10.1144/gsjgs.143.1.0141

    Article  Google Scholar 

  • Hirschmann G, Okrusch M (1988) The Spessart and the Ruhla crystalline complexes as constituent of the central German Crystalline Rise—a correlation. Neues Jahrb Geol Palaontol Abh 177:1–39

    Google Scholar 

  • Le Corre C, Balé P, Geoget Y (1989) Le Léon: un domaine exotique au Nord-Ouest de la chaîne varisque armoricaine. Geodin Acta 3:57–71

    Google Scholar 

  • Le Corre C, Auvray B, Ballevre M, Robardet M (1991) Le Massif Armoricain. Sci Geol Bull 44:31–103

    Google Scholar 

  • Ledru P, Lardeaux JM, Santallier D, Autran A, Quenardel JM, Floc’h JP, Lerouge G, Maillet N, Marchand J, Ploquin A (1989) Où sont les nappes dans le Massif Central français? Bull Soc Geol Fr 8:605–618

    Google Scholar 

  • Le Gall B (1990) Evidence of an imbricate crustal thrust belt in the southern British Variscides. Contribution of SWAT deep sismic reflection profiling recorded in the English Channel and the Celtic Sea. Tectonics 9:283–302. doi:10.1029/TC009i002p00283

    Article  Google Scholar 

  • Leloix C, Faure M, Feybesse JL (1999) Hercynian polyphase tectonics in north-east French Massif Central: the closure of the Brévenne Devonian-Dinantian rift. Int J Earth Sci 88:409–421. doi:10.1007/s005310050275

    Article  Google Scholar 

  • Leutwein F, Chauris L, Sonet J, Zimmermann JL (1969) Etudes géochronologiques et géotectoniques dans le Nord-Finistère (Massif Armoricain). Sci Terre 14:331–358

    Google Scholar 

  • Ludwig KR (2004) Users manual for ISOPLOT/EX, version 3.1. A geochronological toolkit for Microsoft Excel Berkeley Geochronology Center, Special Publication, vol 4

  • Marchand J (1981) Ecaillage d’un “mélange tectonique” profond: le complexe cristallophyllien de Champtoceaux (Bretagne Méridionale). C R Acad Sci Paris II 293:223–228

    Google Scholar 

  • Matte P (1986) La chaîne Varisque parmi les chaînes Paléozoïques périatlantiques, modèle d’évolution et position des grands blocs continentaux au Permo-Carbonifère. Bull Soc Geol Fr 2:9–24

    Google Scholar 

  • Matte P (2001) The Variscan collage and orogeny (480–290 Ma) and the tectonic definition of the Armorica microplate: a review. Terra Nova 13:122–128. doi:10.1046/j.1365-3121.2001.00327.x

    Article  Google Scholar 

  • Matte P, Hirn A (1988) Généralités sur la chaîne varisque d’Europe, coupe complete de la chaîne sous l’Ouest de la France, Programme ECORS Profil Nord de la France. Technip, Paris, pp 197–222

  • Montel JM, Forest S, Veschambree M, Nicollet C, Provost A (1996) Electron microprobe dating of monazite. Chem Geol 131:37–53. doi:10.1016/0009-2541(96)00024-1

    Article  Google Scholar 

  • Montel JM, Kornprobst J, Vielzeuf D (2000) Preservation of old U–Th–Pb ages in shielded monazite: example from Beni Bousera Hercynian Kinzigites (Morroco). J Metamorph Geol 18:335–342

    Article  Google Scholar 

  • Oncken O (1997) Transformation of a magmatic arc and an orogenic root during oblique collision and its consequences for the evolution of the European Variscides (Mid-German Crystalline Rise). Geol Rundsch 86:2–20. doi:10.1007/s005310050118

    Article  Google Scholar 

  • Paquette JL, Balé P, Ballèvre M, Georget Y (1987) Geochronology et géochimie des eclogites du Léon: nouvelles contraintes sur l’évolution géodynamique du Nord-Ouest du Massif Armoricain. Bull Miner 110:683–696

    Google Scholar 

  • Paris F, Robardet M (1990) Early Paleozoic paleobiogeography of the Variscan regions. Tectonophysics 177:193–213

    Article  Google Scholar 

  • Parrish RR (1990) U–Pb dating of monazite and its application to geological problems. Can J Earth Sci 27:1431–1450

    Google Scholar 

  • Pin C (1990) Variscans oceans: ages, origins and geodynamic implications inferred from geochemical and radiometric data. Tectonophysics 177:215–227

    Article  Google Scholar 

  • Pommier A, Cocherie A, Legendre O (2002) EPMA dating users manual-age calculation from electron probe microanalyser measurements of U–Th–Pb, internal report, BRGM, Orleans, 9 pp

  • Pyle JM, Spear FS, Rudnick RL, McDonough WF (2001) Monazite–xenotime–garnet equilibrium in metapelites and a new monazite–garnet thermometer. J Petrol 42:2083–2107

    Article  Google Scholar 

  • Robardet M (2003) The Armorica microplate: fact or fiction? Critical review of the concept and contradictory palaeobiogeographical data. Paleogeogr Palaeoclimatol Palaeoecol 195:125–148

    Article  Google Scholar 

  • Rolet J, Le Gall B, Darboux JR, Thonon P, Gravelle M (1986) L’évolution géodynamique dévono-carbonifère de l’extrémité occidentale de la chaîne hercynienne d’europe sur le transect Armorique-Cornwall. Bull Soc Geol Fr 8:43–54

    Google Scholar 

  • Rolet J, Gresselin F, Jegouzo P, Ledru P, Wyns R (1994) Intracontinental Hercynian events in the Armorican Massif. In: Keppie JD (ed) Pre-Mezozoic geology of France and related areas. Springer, Berlin, pp 195–219

    Google Scholar 

  • Schultz B, De Wall H, Finger F (2007) Continuous variscan deformation during granitoid intrusion in the Léon Domain (Armorican Massif, France). In: Mechanics of Variscan orogeny, September 13–15, 2007, BRGM, Orleans (special volume of Géologie de la France), vol 2, pp 155

  • Suzuki K, Adachi M (1991) The Chemical Th–U–total Pb isochron ages of zircon and monazite from the gray granite of Hida Terrane, Japan. J Earth Sci Nagoya Univ 38:11–37

    Google Scholar 

  • Tait J, Bachtadse V, Franke W, Soffel HC (1997) Geodynamic evolution of the European Variscan fold belt: palaeomagnetic and geological constraints. Geol Rundsch 86:585–598

    Article  Google Scholar 

  • Tera F, Wasserburg GJ (1972) U–Th–Pb systematics in three Apollo 14 basalts and the problem of initial Pb in lunar rocks. Earth Planet Sci Lett 14:281–304

    Article  Google Scholar 

  • Von Raumer J, Stampfli G, Borel G, Bussy F (2002) The organization of pre-Variscan basement areas at the north-Gondwana margin. Int J Earth Sci 91:35–52

    Article  Google Scholar 

  • Wendt I, Carl C (1991) The statistical distribution of the mean squared weighted deviation. Chem Geol 86:275–285

    Google Scholar 

  • Will T, Schmädicke E (2001) A first find of retrogressed eclogites in the Odenwald Crystalline Complex, Mid-German Crystalline Rise, Germany: evidence for a so far unrecognized high-pressure metamorphism in the Central Variscides. Lithos 59:109–125

    Article  Google Scholar 

  • Williams ML, Jercinovic MJ (2002) Microprobe monazite geochronology: putting absolute time into microstructural analysis. J Struct Geol 24:1013–1028

    Article  Google Scholar 

Download references

Acknowledgments

LA ICP MS analyses have been supported by the program “Cartographie géologique de la France au 1/50000” directed by P. Rossi in BRGM (Orléans, France). Constructive reviews by G. Eisbacher, M. Sintubin, and R. Greiling are greatly acknowledged.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Michel Faure.

Rights and permissions

Reprints and permissions

About this article

Cite this article

Faure, M., Sommers, C., Melleton, J. et al. The Léon Domain (French Massif Armoricain): a westward extension of the Mid-German Crystalline Rise? Structural and geochronological insights. Int J Earth Sci (Geol Rundsch) 99, 65–81 (2010). https://doi.org/10.1007/s00531-008-0360-x

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00531-008-0360-x

Keywords

Navigation