Abstract
The island of Corsica, which belongs to the southern Variscan realm, was detached from southern France in the Tertiary. Alongside Alpine and Variscan edifices, it carries outliers of Neoproterozoic metasediments and Lower Paleozoic siliciclastics including Ordovician sandstone and conglomerates as well as Hirnantian diamictites in its NW sector. We investigated the U–Pb–Hf of detrital zircons of basement metasediments and overlying Ordovician sandstone and channeling conglomerate to constrain their provenance, the timing of their deposition, and to deduce the late Ediacaran to Ordovician paleogeography. The youngest detrital zircons in the metasediments are 0.55–0.53 Ga indicating their maximum age of deposition is Late Ediacaran to Early Cambrian, thus classifying the Corsica basement metasediments as Cadomian. The U–Pb analyses revealed that a preponderance of the detrital zircons in the basement micaschist and quartzite portray Neoproterozoic ages concentrating between 0.55 and 0.65 Ga. This is partly consistent with derivation from Pan-African terranes of north Africa yet the presence of detrital zircons younger than ~ 0.6 Ga indicates significant input from Cadomian magmatic arcs that resided within or at the margin of the Cadomian basin in which the metasediments of Corsica were deposited. εHf values of the Ediacaran zircons varies between samples, indicating the provenance comprised both, juvenile arcs and magmatic arcs that involved various degrees of mixing with old crustal components. The Hf-TDM ages of many of the Ediacaran-aged zircons point to a plausible involvement of Meso-Paleoproterozoic crust in the generation of these Cadomian arcs. The presence of small but fairly distinguished populations of Mesoproterozoic-aged (1.0–1.6 Ga) as well as 2.0–2.2 Ga and 2.4–2.6 Ga detrital zircons in the Cadomian metasediments farther indicates the presence of such crust in the provenance. Although Mesoproterozoic detrital zircons are usually considered the hallmark of Avalonian terranes, the presence of Hirnantian glacial sediments at the Corsican sequence indicates it resided in the vicinity of Gondwana. We therefore postulate that the Pre-Neoproterozoic zircons have sourced from exotic crustal vestiges that were entrained and accreted within the Cadomian realm itself. The transition into the overlying Ordovician sandstone and conglomerate marks a major change in the provenance, possibly pointing to lateral motions along the strike of the peripheral Cadomian domain. The youngest concordant detrital zircon in the Ordovician (“Ciuttone”) sandstone yielded an age of 0.48 Ga. The detrital zircon ages define an overwhelming concentration at 0.55 Ga, indicating the source of the Ordovician sandstone was cut off from the Gondwana hinterland and that sand was exclusively derived from a latest Ediacaran arc. In view of the sharp detrital zircon age peak, the Corsica Ordovician sandstone cannot be straightforwardly correlated with Armorican sandstone because the detrital zircon spectra of the latter are generally broader, indicating derivation from various sectors of the North Gondwana crust. εHf(t) values of the 0.55 Ga zircons are mostly positive and the corresponding TDM ages at 0.7–1.2 Ga indicating derivation from a juvenile island arc. While TDM ages of this type are common for late Ediacaran Avalonian rocks, the presence of Hirnantian diamictite in Corsica further substantiates that the aforementioned 0.55 Ga island arc evolved in the peripheral Cadomian realm. As a whole, the U–Pb–Hf zircon data from the Corsica sequences reveal the presence of juvenile Cadomian arcs alongside Cadomian arcs that recycled ancient (pre-Neoproterozoic) crust. Along strike variations of this type are known from the Japanese islands, in line with the peripheral Cadomian orogeny being an ancient analog of a Western-Pacific type plate boundary.
Similar content being viewed by others
References
Abati J, Aghzer AM, Gerdes A, Ennih N (2012) Insights on the crustal evolution of the West African Craton from Hf isotopes in detrital zircons from the Anti-Atlas belt. Precambrian Res 212:263–274. https://doi.org/10.1016/j.precamres.2012.06.005 doi
Abbo A, Avigad D, Gerdes A, Güngör T (2015) Cadomian basement and Paleozoic to Triassic siliciclastics of the Taurides (Karacahisar dome, south-central Turkey): paleogeographic constraints from U–Pb–Hf in zircons. Lithos 227:122–139. https://doi.org/10.1016/j.lithos.2015.03.023
Albert R, Arenas R, Gerdes A et al (2014) Provenance of the Variscan Upper Allochthon (Cabo Ortegal Complex, NW Iberian Massif). Gondwana Res. https://doi.org/10.1016/j.gr.2014.10.016
Avigad D, Gerdes A, Morag N, Bechstadt T (2012) Coupled U–Pb–Hf of detrital zircons of Cambrian sandstones from Morocco and Sardinia: implications for provenance and Precambrian crustal evolution of North Africa. Gondwana Res 21:690–703. https://doi.org/10.1016/J.Gr.2011.06.005 doi
Avigad D, Abbo A, Gerdes A (2016) Origin of the eastern mediterranean: Neotethys rifting along a cryptic cadomian suture with Afro-Arabia. Bull Geol Soc Am. https://doi.org/10.1130/B31370.1
Bahlburg H, Vervoort JD, DuFrane SA (2010) Plate tectonic significance of Middle Cambrian and Ordovician siliciclastic rocks of the Bavarian Facies, Armorican Terrane Assemblage, Germany—U–Pb and Hf isotope evidence from detrital zircons. Gondwana Res 17:223–235. https://doi.org/10.1016/j.gr.2009.11.007
Ballèvre M, Le Goff E, Hébert R (2001) The tectonothermal evolution of the Cadomian belt of northern Brittany, France: a Neoproterozoic volcanic arc. Tectonophysics 331:19–43. https://doi.org/10.1016/S0040-1951(00)00234-1
Barca S, Durand-Delga M, Rossi P, Storch P (1996) Les micaschistes panafricains de Corse et leur couverture paleozoique; leur interpretation au sein de l’orogene varisque sud-europeen. Comptes Rendues Acad Sci Paris 322:981–989
Bard J-P (1997) Démembrement anté-mésozoïque de la chaîne varisque d’Europe occidentale et d’Afrique du Nord: rôle essentiel des grands décrochements transpressifs dextres accompagnant la rotation-translation horaire de l’Afrique durant le Stéphanien. Comptes Rendus l’Académie des Sci Série 2 Sci la terre des planètes 324:693–704
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. https://doi.org/10.1016/j.epsl.2010.07.012
Bouvier A, Vervoort JD, Patchett PJ (2008) The Lu–Hf and Sm–Nd isotopic composition of CHUR: constraints from unequilibrated chondrites and implications for the bulk composition of terrestrial planets. Earth Planet Sci Lett 273:48–57. https://doi.org/10.1016/j.epsl.2008.06.010 doi
Calvez JY, Vidal P (1978) Two billion years old relicts in the Hercynian Belt of western Europe. Contrib to Mineral Petrol 65:395–399
Chantraine J, Egal E, Thiéblemont D et al (2001) The Cadomian active margin (North Armorican Massif, France): a segment of the North Atlantic Panafrican belt. Tectonophysics 331:1–18. https://doi.org/10.1016/S0040-1951(00)00233-X
Chelle-Michou C, Laurent O, Moyen J-F et al (2017) Pre-Cadomian to late-Variscan odyssey of the eastern Massif Central, France: formation of the West European crust in a nutshell. Gondwana Res 46:170–190. https://doi.org/10.1016/j.gr.2017.02.010
Couzinié S, Laurent O, Poujol M et al (2017) Cadomian S-type granites as basement rocks of the Variscan belt (Massif Central, France): implications for the crustal evolution of the north Gondwana margin. Lithos 286–287:16–34. https://doi.org/10.1016/j.lithos.2017.06.001
Díez Fernández R, Martínez Catalán JR, Arenas R et al (2012) 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 Lond 169:655–665. https://doi.org/10.1144/jgs2011-146
Dörr W, Fiala J, Vejnar Z, Zulauf G (1998) U–Pb zircon ages and structural development of metagranitoids of the Tepla crystalline complex: evidence for pervasive Cambrian plutonism within the Bohemian Massif (Czech Republic). Geol Rundschau 87:135–149. https://doi.org/10.1007/s005310050195
Dörr W, Zulauf G, Gerdes A et al (2015) A hidden Tonian basement in the eastern Mediterranean: age constraints from U–Pb data of magmatic and detrital zircons of the External Hellenides (Crete and Peloponnesus). Precambrian Res 258:83–108. https://doi.org/10.1016/j.precamres.2014.12.015
Drost K, Gerdes A, Jeffries T et al (2011) Provenance of Neoproterozoic and early Paleozoic siliciclastic rocks of the Tepla-Barrandian unit (Bohemian Massif): evidence from U–Pb detrital zircon ages. Gondwana Res 19:213–231. https://doi.org/10.1016/J.Gr.2010.05.003 doi
Durand-Delga M, Rossi P (1991) Les massifs anciens de la France: la Corse. Sci Géol Mém Strasbg 44:311–336
Edel J-B, Casini L, Oggiano G et al (2014) Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise rotation. Geol Soc Lond Spec Publ 405:333–361. https://doi.org/10.1144/SP405.10
Faure M, Rossi P, Gaché J et al (2014) Variscan orogeny in Corsica: new structural and geochronological insights, and its place in the Variscan geodynamic framework. Int J Earth Sci 103:1533–1551. https://doi.org/10.1007/s00531-014-1031-8
Fernández-Suárez J, Gutiérrez-Alonso G, Jenner G, Tubrett MN (2000) New ideas on the Proterozoic-Early Palaeozoic evolution of NW Iberia: Insights from U–Pb detrital zircon ages. Precambrian Res 102:185–206. https://doi.org/10.1016/S0301-9268(00)00065-6
Friedl G, Finger F, McNaughton NJ, Fletcher IR (2000) Deducing the ancestry of terranes: SHRIMP evidence for South America-derived Gondwana fragments in central Europe. Geology 28:1035–1038. https://doi.org/10.1130/0091-7613(2000)28%3C1035:DTAOTS%3E2.0.CO;2
Friedl G, Finger F, Paquette JL et al (2004) Pre-Variscan geological events in the Austrian part of the Bohemian Massif deduced from U–Pb zircon ages. Int J Earth Sci 93:802–823. https://doi.org/10.1007/s00531-004-0420-9 doi
Gasquet D, Levresse G, Cheilletz A et al (2005) Contribution to a geodynamic reconstruction of the Anti-Atlas (Morocco) during Pan-African times with the emphasis on inversion tectonics and metallogenic activity at the Precambrian–Cambrian transition. Precambrian Res 140:157–182. https://doi.org/10.1016/j.precamres.2005.06.009
Gasquet D, Ennih N, Liégeois J-P et al (2008) The Pan-African Belt. In: Continental evolution: the geology of Morocco. Springer, New York, pp 33–64
Gattacceca J, Deino A, Rizzo R et al (2007) Miocene rotation of Sardinia: new paleomagnetic and geochronological constraints and geodynamic implications. Earth Planet Sci Lett 258:359–377. https://doi.org/10.1016/j.epsl.2007.02.003
Gebauer D, Friedl G (1994) A 1.38 Ga protolith age for the Dobra orthogneiss (Moldanubian Zone of the southern Bohemian Massif, NE-Austria): evidence from ion-microprobe (SHRIMP) dating of zircon. J Czech Geol Soc 39:34–35
Gebauer D, Williams IS, Compston W, Grünenfelder M (1989) The development of the Central European continental crust since the Early Archaean based on conventional and ion-microprobe dating of up to 3.84 b.y. old detrital zircons. Tectonophysics 157:81–96. https://doi.org/10.1016/0040-1951(89)90342-9
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 Annorican metasediment in Central Germany. Earth Planet Sci Lett 249:47–61. https://doi.org/10.1016/j.epsl.2006.06.039 doi
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 Central Zone of the Limpopo Belt. Chem Geol 261:230–243. https://doi.org/10.1016/j.chemgeo.2008.03.005 doi
Guillot S, Ménot R-P (2009) Paleozoic evolution of the external crystalline massifs of the Western Alps. Comptes Rendus Geosci 341:253–265
Gutierrez-Alonso G, Fernandez-Suarez J, Collins AS et al (2005) Amazonian Mesoproterozoic basement in the core of the Ibero-Armorican Arc: 40Ar/39Ar detrital mica ages complement the zircon’s tale. Geology 33:637–640. https://doi.org/10.1130/G21485.1
Gutiérrez-Alonso G, Fernández-Suárez J, Jeffries TE et al (2003) Terrane accretion and dispersal in the northern Gondwana margin. An Early Paleozoic analog of a long-lived active margin. Tectonophysics 365:221–232. https://doi.org/10.1016/S0040-1951(03)00023-4
Gutiérrez-Alonso G, Fernández-Suárez J, Gutiérrez-Marco JC et al (2007) U–Pb depositional age for the upper Barrios Formation (Armorican Quartzite facies) in the Cantabrian zone of Iberia: Implications for stratigraphic correlation and paleogeography. Spec Pap Soc Am 423:287
Hajná J, Žák J, Dörr W (2017) Time scales and mechanisms of growth of active margins of Gondwana: a model based on detrital zircon ages from the Neoproterozoic to Cambrian Blovice accretionary complex, Bohemian Massif. Gondwana Res 42:63–83. https://doi.org/10.1016/j.gr.2016.10.004
Henderson BJ, Collins WJ, Murphy JB et al (2016) Gondwanan basement terranes of the Variscan–Appalachian orogen: Baltican, Saharan and West African hafnium isotopic fingerprints in Avalonia, Iberia and the Armorican Terranes. Tectonophysics 681:278–304. https://doi.org/10.1016/j.tecto.2015.11.020
Inglis JD, Samson SD, D’Lemos RS, Hamilton M (2004) U–Pb geochronological constraints on the tectonothermal evolution of the Paleoproterozoic basement of Cadomia, la Hague, NW France. Precambrian Res 134:293–315. https://doi.org/10.1016/j.precamres.2004.07.003
Isozaki Y, Maruyama S, Nakama T, Yamamoto S, Yanai S (2011) Growth and shrinkage of an active continental margin: updated geotectonic history of the japanese islands. J Geogr (Chigaku Zasshi) 120(1):65–99
Jackson SE, Pearson NJ, Griffin WL, Belousova EA (2004) The application of laser ablation-inductively coupled plasma-mass spectrometry to in situ U–Pb zircon geochronology. Chem Geol 211:47–69. https://doi.org/10.1016/j.chemgeo.2004.06.017 doi
Jahn BM (2010) Accretionary orogen and evolution of the Japanese Islands-implications from a Sr–Nd isotopic study of the phanerozoic granitoids from SW Japan. Am J Sci 310:1210–1249. https://doi.org/10.2475/10.2010.02
Jahn BM, Usuki M, Usuki T, Chung SL (2014) Generation of cenozoic granitoids in hokkaido (JAPAN): constraints from zircon geochronology, Sr-Nd-Hf ISOTOPIC and geochemical analyses, and implications for crustal growth. Am J Sci 314:704–750. https://doi.org/10.2475/02.2014.09
Keay S, Lister G (2002) African provenance for the metasediments and metaigneous rocks of the Cyclades, Aegean Sea, Greece. Geology 30:235–238. https://doi.org/10.1130/0091-7613(2002)030<0235:APFTMA>2.0.CO;2
Košler J, Konopásek J, Sláma J, Vrána S (2014) U–Pb zircon provenance of Moldanubian metasediments in the Bohemian Massif. J Geol Soc Lond 171:83–95. https://doi.org/10.1144/jgs2013-059
Linnemann U, Gerdes A, Drost K, Buschmann B (2007) The continuum between Cadomian orogenesis and opening of the Rheic Ocean: constraints from LA-ICP-MS U–Pb zircon dating and analysis of plate-tectonic setting (Saxo-Thuringian zone, northeastern Bohemian Massif, Germany). Geol Soc Am Spec Pap 423:61–96. https://doi.org/10.1130/2007.2423(03)
Linnemann U, D’Lemos R, Drost K et al (2008a) Cadomian tectonics. In: McCann T (ed) The geology of Central Europe—Volume 1: Precambrian and Palaeozoic. The Geological Society of London, London, pp 103–154
Linnemann U, Pereira F, Jeffries TE et al (2008b) The Cadomian Orogeny and the opening of the Rheic Ocean: The diacrony of 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. https://doi.org/10.1016/j.tecto.2008.05.002 doi
Linnemann U, Romer R, Pin C et al (2008c) Precambrian. In: McCann T (ed) The geology of Central Europe—Volume 1: Precambrian and Palaeozoic. The Geological Society of London, London, pp 21–101
Linnemann U, Gerdes A, Hofmann M, Marko L (2014) The Cadomian Orogen: Neoproterozoic to Early Cambrian crustal growth and orogenic zoning along the periphery of the West African Craton—Constraints from U–Pb zircon ages and Hf isotopes (Schwarzburg Antiform, Germany). Precambrian Res 244:236–278. https://doi.org/10.1016/j.precamres.2013.08.007
Martinez Catalan JR, Fernandez-Suarez J, Jenner GA et al (2004) Provenance constraints from detrital zircon U–Pb ages in the NW Iberian Massif: implications for Palaeozoic plate configuration and Variscan evolution. J Geol Soc London 161:463–476. https://doi.org/10.1144/0016-764903-054
Matte P (2001) The Variscan collage and orogeny (480–290 Ma) and the tectonic definition of the Armorica microplate: a review. Terra Nov 13:122–128
Meinhold G, Morton AC, Avigad D (2013) New insights into peri-Gondwana paleogeography and the Gondwana super-fan system from detrital zircon U–Pb ages. Gondwana Res 23:661–665. https://doi.org/10.1016/J.Gr.2012.05.003 doi
Morag N, Avigad D, Gerdes A et al (2011) Crustal evolution and recycling in the northern Arabian-Nubian Shield: New perspectives from zircon Lu–Hf and U–Pb systematics. Precambrian Res 186:101–116. https://doi.org/10.1016/j.precamres.2011.01.004 doi
Murphy JB, Nance RD (2002) Sm–Nd isotopic systematics as tectonic tracers: an example from West Avalonia in the Canadian Appalachians. Earth-Science Rev 59:77–100. https://doi.org/10.1016/S0012-8252(02)00070-3
Nance RD, Murphy JB, Strachan RA et al (2008) Neoproterozoic-early Palaeozoic tectonostratigraphy and palaeogeography of the peri-Gondwanan terranes: Amazonian v. West African connections. Geol Soc Lond Spec Publ 297:345–383. https://doi.org/10.1144/sp297.17
Noblet C, Lefort JP (1990) Sedimentological evidence for a limited separation between Armorica and Gondwana during the Early Ordovician. Geol 18:303–306. https://doi.org/10.1130/0091-7613(1990)018<0303:SEFALS>2.3.CO;2
Orejana D, Merino Martínez E, Villaseca C, Andersen T (2015) Ediacaran–Cambrian paleogeography and geodynamic setting of the Central Iberian Zone: constraints from coupled U–Pb–Hf isotopes of detrital zircons. Precambrian Res 261:234–251. https://doi.org/10.1016/j.precamres.2015.02.009
Pereira MF, Chichorro M, Williams IS, Silva JB (2008) Zircon U–Pb geochronology of paragneisses and biotite granites from the SW Iberian Massif (Portugal): evidence for a palaeogeographical link between the Ossa–Morena Ediacaran basins and the West African craton. Geol Soc London Spec Publ 297:385–408. https://doi.org/10.1144/SP297.18
Pereira MF, Sola AR, Chichorro M et al (2012) North-Gondwana assembly, break-up and paleogeography: U–Pb isotope evidence from detrital and igneous zircons of Ediacaran and Cambrian rocks of SW Iberia. Gondwana Res 22:866–881. https://doi.org/10.1016/J.Gr.2012.02.010 doi
Rossi P, Lahondère JC, Lluch D et al (1994) Carte Géologique de France 1: 50.000; feuille Saint Florent (1103). Not Explic BRGM, Orléans 93
Rossi P, Cocherie A, Durand-Delga M (1995) Arguments géochronologiques en faveur de la présence d’un socle panafricain (cadomien) en Corse, conséquences sur la paléogéographie de l’orogène varisque sud-européen. Comptes Rendus l’Académie des Sci Série 2 Sci la terre des planètes 321:983–992
Rossi Ph, Durand-Delga M, Lahondère J-C et al (2000) Carte géol. France à 1/50 000, feuille Santo-Pietro-di-Tenda (1106) – Orléans : BRGM. Notice explicative par Ph. Rossi, M. Durand-Delga, J-C. Lahondère, D. Lahondère, 2000
Rossi P, Oggiano G, Cocherie A (2009) A restored section of the “southern Variscan realm” across the Corsica–Sardinia microcontinent. Comptes Rendus Geosci 341:224–238
Sagawe A, Gärtner A, Linnemann U et al (2016) Exotic crustal components at the northern margin of the Bohemian Massif—implications from U[sbnd]Th[sbnd]Pb and Hf isotopes of zircon from the Saxonian Granulite Massif. Tectonophysics 681:234–249. https://doi.org/10.1016/j.tecto.2016.04.013
Samson SD, D’Lemos RS, Miller BV, Hamilton M (2005) Neoproterozoic palaeogeography of the Cadomia and Avalon terranes: constraints from detrital zircon U–Pb ages. J Geol Soc London 162:65–71. https://doi.org/10.1144/0016-764904-003
Scherer E, Munker C, Mezger K (2001) Calibration of the lutetium-hafnium clock. Science 293:683–687. https://doi.org/10.1126/science.1061372 doi
Shaw J, Gutiérrez-Alonso G, Johnston ST, Pastor Galán D (2014) Provenance variability along the Early Ordovician north Gondwana margin: Paleogeographic and tectonic implications of U–Pb detrital zircon ages from the Armorican Quartzite of the Iberian Variscan belt. Bull Geol Soc Am 126:702–719. https://doi.org/10.1130/B30935.1
Söderlund U, Patchett PJ, Vervoort JD, Isachsen CE (2004) The 176 Lu decay constant determined by Lu–Hf and U–Pb isotope systematics of Precambrian mafic intrusions. Earth Planet Sci Lett 219:311–324
Soulaimani A, Piqué A (2004) The Tasrirt structure (Kerdous inlier, Western Anti-Atlas, Morocco): a late Pan-African transtensive dome. J African Earth Sci 39:247–255
Soulaimani A, Bouabdelli M, Piqué A (2003) L’extension continentale au Néo-Protérozoïque supérieur-Cambrien inférieur dans l’Anti-Atlas (Maroc). Bull Soc Geol Fr 174:83–92. https://doi.org/10.2113/174.1.83
Stacey JS, Kramers JD (1975) Approximation of Terrestrial Lead Isotope Evolution by a 2-Stage Model. Earth Planet Sci Lett 26:207–221. https://doi.org/10.1016/0012-821x(75)90088-6 doi
Stam JC (1952) Géologie de la région du Tenda Septentrional (Corse). Universiteit van Amsterdam
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. https://doi.org/10.1016/S0012-821x(01)00588-X
Stampfli GM, von Raumer JF, Borel GD (2002) Paleozoic evolution of pre-Variscan terranes: from Gondwana to the Variscan collision. Spec Pap Soc Am 263–280
Stampfli GM, Von Raumer J, Wilhem C (2011) The distribution of Gondwana-derived terranes in the early paleozoic. In: Gutiérrez-Marco JC, Rábano I, García-Bellido D (eds) Ordovician of the World. IGME, Madrid, pp 567–574
Stern RA, Bodorkos S, Kamo SL et al (2009) Measurement of SIMS instrumental mass fractionation of Pb isotopes during zircon dating. Geostand Geoanalytical Res 33:145–168
Termier P, Maury E (1928) Nouvelles observations géologiques dans la Corse orientale. Comptes-Rendus l’Académie des Sci Paris 186:1324–1327
Vermeesch P (2012) On the visualisation of detrital age distributions. Chem Geol 312–313:190–194. https://doi.org/10.1016/j.chemgeo.2012.04.021
von Raumer J, Stampfli G, Borel G, Bussy F (2002) Organization of pre-Variscan basement areas at the north-Gondwanan margin. Int J Earth Sci 91:35–52. https://doi.org/10.1007/s005310100200
von Raumer JF, Stampfli GA, Bussy F (2003) Gondwana-derived microcontinents - the constituents of the Variscan and Alpine collisional orogens. Tectonophysics 365:7–22. https://doi.org/10.1016/S0040-1951(03)00015-5 doi
Wendt JI, Kröner A, Fiala J, Todt W (1993) Evidence from zircon dating for existence of approximately 2.1 Ga old crystalline basement in southern Bohemia, Czech Republic. Geol Rundschau 82:42–50. https://doi.org/10.1007/BF00563269
Wiedenbeck M, Allé P, Corfu F et al (1995) Three Natural Zircon Standards for U-Th-Pb, Lu-Hf, Trace Element and REE Analyses. Geostand Newsl 19:1–23. https://doi.org/10.1111/j.1751-908X.1995.tb00147.x
Woodhead JD, Hergt JM (2005) A preliminary appraisal of seven natural zircon reference materials for in situ Hf isotope determination. Geostand Geoanalytical Res 29:183–195
Zeh A, Gerdes A (2010) Baltica- and Gondwana-derived sediments in the Mid-German Crystalline Rise (Central Europe): Implications for the closure of the Rheic ocean. Gondwana Res 17:254–263. https://doi.org/10.1016/j.gr.2009.08.004
Zlatkin O, Avigad D, Gerdes A (2013) Evolution and provenance of Neoproterozoic basement and Lower Paleozoic siliciclastic cover of the Menderes Massif (western Taurides): Coupled U–Pb-Hf zircon isotope geochemistry. Gondwana Res 23:682–700. https://doi.org/10.1016/J.Gr.2012.05.006 doi
Zlatkin O, Avigad D, Gerdes A (2014) Peri-Amazonian provenance of the Proto-Pelagonian basement (Greece), from zircon U–Pb geochronology and Lu-Hf isotopic geochemistry. Lithos 184:379–392. https://doi.org/10.1016/j.lithos.2013.11.010 doi
Zulauf G, Dörr W, Fiala J, Vejnar Z (1997) Late Cadomian crustal tilting and Cambrian transtension in the Teplá–Barrandian unit (Bohemian Massif, Central European Variscides). Geol Rundschau 86:571–584. https://doi.org/10.1007/s005310050164
Zulauf G, Romano SS, Dörr W, Fiala J (2007) Crete and the Minoan terranes: Age constraints from U–Pb dating of detrital zircons. Geol Soc Am Spec Pap 423:401–411. https://doi.org/10.1130/2007.2423(19
Acknowledgements
This research was supported by the G.I.F., the German–Israeli Foundation for Scientific Research and Development (Grant Number 1248-301.8/2014). We thank O. Zlatkin for carrying the analytical measurements on #Cor-1, to Y. Geller for technical assistance and to L. Marko for invaluable analytical support at GUF. We thank Jiří Žák for guiding us on a fieldtrip to the Bohemian Massif in the frame of Erasmus cooperation. Reviews by M. Faure and C. Chelle-Michou helped to improve this manuscript and are greatly acknowledged.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Avigad, D., Rossi, P., Gerdes, A. et al. Cadomian metasediments and Ordovician sandstone from Corsica: detrital zircon U–Pb–Hf constrains on their provenance and paleogeography. Int J Earth Sci (Geol Rundsch) 107, 2803–2818 (2018). https://doi.org/10.1007/s00531-018-1629-3
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00531-018-1629-3