Skip to main content
SpringerLink
Log in

Long-lasting Cadomian magmatic activity along an active northern Gondwana margin: U–Pb zircon and Sr–Nd isotopic evidence from the Brunovistulian Domain, eastern Bohemian Massif

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

Abstract

Cadomian magmatic complexes of the Brunovistulian Domain crop out at the eastern termination of the Bohemian Massif. However, the age, nature and geotectonic affinity of some of pre-Variscan (meta-)igneous rock complexes from this domain are still unknown. Geochronological and geochemical study of the granitic rocks across the Brunovistulian Domain reveals new information about the timing and nature of this magmatic activity originally situated along the northern margin of Gondwana. Zircon U–Pb data (601 ± 3 Ma, Brno Massif; 634 ± 6 Ma, paraautochtonous core of the Svratka Dome; 568 ± 3 Ma, Bíteš orthogneiss) from the allochtonous Moravicum indicate the prolonged magmatic activity within the Brunovistulian Domain during the Ediacaran. The major- and trace-element and Sr–Nd isotopic signatures show heterogeneous geochemical characteristics of the granitic rocks and suggest a magmatic-arc geotectonic setting. The two-stage Depleted Mantle Nd model ages (c. 1.3–2.0 Ga) indicate derivation of the granitic rocks from a relatively primitive crustal source, as well as from an ancient and evolved continental crust of the Brunovistulian Domain. These results constrain the magmatic-arc activity to c. 635–570 Ma and provide a further evidence for a long-lived (at least c. 65 Myr) and likely episodic subduction-related magmatism at the northern margin of Gondwana. The presence of granitic intrusions derived from variously mature crustal sources at different times suggests heterogeneous crustal segments to having been involved in the magmatic-arc system during its multistage evolution.

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

Access this article

Log in via an institution

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

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

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1
Fig. 2
Fig. 3
Fig. 4
Fig. 5
Fig. 6
Fig. 7
Fig. 8
Fig. 9
Fig. 10
Fig. 11

Similar content being viewed by others

References

  • Albert R, Arenas R, Gerdes A, Sánchez Martínez S, Marko L (2015a) Provenance of the HP-HT subducted margin in the Variscan belt (Cabo Ortegal Complex, NW Iberian Massif). J Metamorph Geol 33:959–979

    Article  Google Scholar 

  • Albert R, Arenas R, Gerdes A, Sánchez Martínez S, Fernández-Suárez J, Fuenlabrada JM (2015b) Provenance of the Variscan Upper Allochthon (Cabo Ortegal Complex, NW Iberian Massif). Gondwana Res 28:1434–1448

    Article  Google Scholar 

  • Bandres A, Eguiluz L, Gil Ibarguchi JI, Palacios T (2002) Geodynamic evolution of a Cadomian arc region: the northern Ossa-Morena zone, Iberian Massif. Tectonophysics 352:105–120

    Article  Google Scholar 

  • Belka Z, Valverde-Vaquero P, Dörr W, Ahrendt H, Wemmer K, Franke W, Schäer J (2002) Accretion of first Gondwana-derived terranes at the margin of Baltica. In: Winchester JA, Pharaoh TC, Verniers J (eds) Palaeozoic Amalgamation of Central Europe. Geological Society, London, Special Publications 201:19–36

  • Bingen B, Belousova EA, Griffin WL (2011) Neoproterozoic recycling of the Sveconorwegian orogenic belt: detrital-zircon data from the Sparagmite basins in the Scandinavian Caledonides. Precambr Res 189:347–367

    Article  Google Scholar 

  • Boynton WV (1984) Cosmochemistry of the rare earth elements: meteorite studies. In: Henderson P (ed) Rare Earth Element Geochemistry. Elsevier, Amsterdam, pp 63–114

    Chapter  Google Scholar 

  • Cardona A, Cordani UG, Ruiz J, Valencia VA, Armstrong R, Chew D, Nutman A, Sanchez AW (2009) U–Pb zircon geochronology and Nd isotopic signatures of the Pre-Mesozoic metamorphic basement of the Eastern Peruvian Andes: growth and provenance of a Late Neoproterozoic to Carboniferous accretionary orogen on the northwest margin of Gondwana. J Geol 117:285–305

    Article  Google Scholar 

  • Casas JM, Navidad M, Castiñeiras P, Liesa M, Aguilar C, Carreras J, Hofmann M, Gärtner A, Linnemann U (2015) The Late Neoproterozoic magmatism in the Ediacaran series of the Eastern Pyrenees: new ages and isotope geochemistry. Int J Earth Sci 104:909–925

    Article  Google Scholar 

  • Castiñeiras P, Navidad M, Liesa M, Carreras J, Casas JM (2008) U–Pb zircon ages (SHRIMP) for Cadomian and Early Ordovician magmatism in the Eastern Pyrenees: New insights into the pre-Variscan evolution of the northern Gondwana margin. Tectonophysics 461:228–239

    Article  Google Scholar 

  • Cháb J, Stráník Z, Eliáš M (2007) Geological map of the Czech Republic 1:500 000. Czech Geological Survey, Prague

    Google Scholar 

  • Chantraine J, Egal E, Thieblemont D, Le Goff E, Guerrot C, Ballévre M, Guennoc P (2001) The Cadomian active margin (north Armorican Massif, France): a segment of the North Atlantic Pan-African belt. Tectonophysics 33:1–18

    Article  Google Scholar 

  • Cox KG, Bell JD, Pankhurst RJ (1979) The Interpretation of Igneous Rocks. George Allen & Unwin, London, pp 1–450

    Book  Google Scholar 

  • D’Lemos RS, Strachan RA, Topley CG (1990) The Cadomian Orogeny in the north Armorican Massif: a brief review. In: D’Lemos RS, Strachan RA, Topley CG (eds) The Cadomian orogeny. Geological Society, London, Special Publications 51:3–12

  • Dallmeyer RD, Franke W, Weber K (1995) Pre-Permian geology of Central and Eastern Europe. Springer, Berlin, pp 1–593

    Book  Google Scholar 

  • De La Roche H, Leterrier J, Grandclaude P, Marchal M (1980) A classification of volcanic and plutonic rocks using R 1 R 2-diagram and major element analyses—its relationships with current nomenclature. Chem Geol 29:183–210

    Article  Google Scholar 

  • Debon F, Le Fort P (1983) A chemical–mineralogical classification of common plutonic rocks and associations. Trans R Soc Edinb Earth Sci 73:135–149

    Article  Google Scholar 

  • Dörr W, Fiala J, Vejnar Z, Zulauf G (1998) U–Pb zircon ages and structural development of metagranitoids of the Teplá crystalline complex: evidence for pervasive Cambrian plutonism within the Bohemian Massif (Czech Republic). Geol Rundsch 87:135–149

    Article  Google Scholar 

  • Dörr W, Zulauf G, Fiala J, Franke W, Vejnar Z (2002) Neoproterozoic to Early Cambrian history of an active plate margin in the Teplá–Barrandian Unit—a correlation of U–Pb isotopic-dilution-TIMS ages (Bohemia, Czech Republic). Tectonophysics 352:65–85

    Article  Google Scholar 

  • Dörr W, Zulauf G, Gerdes A, Lahaye Y, Kowalczyk G (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). Precambr Res 258:83–108

    Article  Google Scholar 

  • Drost K, Romer RL, Linnemann U, Fatka O, Kraft P, Marek J (2007) Nd–Sr–Pb isotopic signatures of Neoproterozoic–early Paleozoic siliciclastic rocks in response to changing geotectonic regimes: a case study from the Barrandian area (Bohemian Massif, Czech Republic). In: Linnemann 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 Papers 423, pp 191–208

  • Drost K, Gerdes A, Jeffries T, Linnemann U, Storey C (2011) Provenance of Neoproterozoic and early Paleozoic siliciclastic rocks of the Teplá–Barrandian Unit (Bohemian Massif): evidence from U–Pb detrital zircon ages. Gondwana Res 19:213–231

    Article  Google Scholar 

  • Ducea MN, Saleeby JB, Bergantz G (2015) The architecture, chemistry, and evolution of continental magmatic arcs. Annu Rev Earth Planet Sci 43:299–333

    Article  Google Scholar 

  • Dudek A (1980) The crystalline basement block of the Outer Carpathians in Moravia: BrunoVistulicum. Rozpr Čs Akad Věd 90:3–85

    Google Scholar 

  • Dudek A, Melková J (1975) Radiometric age and isotopic data determination in the crystalline basement of the Carpathian Foredeep and of the Moravian Flysch. Věst Ústř Úst Geol 50:257–264

    Google Scholar 

  • Dunstan LP, Gramlich JW, Barnes IL, Purdy WC (1980) Absolute isotopic abundance and the atomic weight of a reference sample of thallium. J Res Nat Bur Stand 85:1–10

    Article  Google Scholar 

  • Fernández-Suárez J, Gutiérrez-Alonso G, Jenner GA, Tubrett MN (2000) New ideas on the Proterozoic-Early Palaeozoic evolution of NW Iberia: insights from U–Pb detrital zircon ages. Precambr Res 102:185–206

    Article  Google Scholar 

  • Finger F, Pin C (1997) Arc-type crustal zoning in the Brunovistulicum, eastern Czech Republic: a trace of the late Proterozoic Euro-Gondwana margin. J Czech Geol Soc 42:53

    Google Scholar 

  • Finger F, Frasl G, Dudek A, Jelínek E, Thöni M (1995) Igneous activity (Cadomian plutonism in the Moravo-Silesian basement). In: Dallmeyer RD, Franke W, Weber KP (eds) Pre-Permian geology of Central and Eastern Europe. Springer, Berlin, pp 495–507

    Chapter  Google Scholar 

  • Finger F, von Quadt A, Pin C, Steyrer HP (1998) The ophiolite chain along the western Moravo-Silesian plate margin—a trace of the Rheic suture? Acta Univ Carol Geol 42:244–245

    Google Scholar 

  • Finger F, Hanžl P, Pin C, von Quadt A, Steyrer HP (2000a) The Brunovistulian: Avalonian Precambrian sequence at the eastern end of the Central European Variscides? In: Franke W, Haak V, Oncken O, Tanner D (eds) Orogenic Processes: Quantification and Modelling in the Variscan Belt. Geological Society, London, Special Publications 179, pp 103–112

  • Finger F, Tichomirowa M, Pin C, Hanžl P (2000b) Relics of early-Panafrican metabasite–metarhyolite formation in the Brno Massif, Moravia, Czech Republic. Int J Earth Sci (Geol Rundsch) 89:328–335

    Article  Google Scholar 

  • Finger F, Gerdes A, Janoušek V, René M, Riegler G (2007) Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo-Moldanubian tectonometamorphic phases. J Geosci 52:9–28

    Google Scholar 

  • 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) Orogenic Processes: Quantification and Modelling in the Variscan Belt. Geological Society, London, Special Publications 179, pp 35–61

  • 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

    Article  Google Scholar 

  • Friedl G, Finger F, Paquette JL, von Quadt A, McNaughton NJ, Fletcher IR (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

    Article  Google Scholar 

  • Fritz H, Dallmeyer RD, Neubauer F (1996) Thick-skinned versus thin-skinned thrusting: rheology controlled thrust propagation in the Variscan collisional belt (the southeastern Bohemian Massif, Czech Republic–Austria). Tectonics 15:1389–1413

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Gürsu S, Goncuoglu MC (2008) Petrogenesis and geodynamic evolution of the Late Neoproterozoic post-collisional felsic magmatism in NE Afyon area, western central Turkey. In: Ennih N, Liégeois J-P (eds) The boundaries of the West African Craton. Geological Society, London, Special Publications 297, pp 409–431

  • Hajná J, Žák J, Kachlík V, Chadima M (2010) Subduction-driven shortening and differential exhumation in a Cadomian accretionary wedge: The Teplá–Barrandian unit, Bohemian Massif. Precambr Res 176:27–45

    Article  Google Scholar 

  • Hajná J, Žák J, Kachlík V, Dörr W, Gerdes A (2013) Neoproterozoic to early Cambrian Franciscan-type mélanges in the Teplá–Barrandian unit, Bohemian Massif: Evidence of modern-style accretionary processes along the Cadomian active margin of Gondwana? Precambr Res 224:653–670

    Article  Google Scholar 

  • Hanžl P, Melichar R (1997) The Brno Massif: a section through the active continental margin of a composed terrane? Krystalinikum 23:33–58

    Google Scholar 

  • Hanžl P, Hrdličková K, Čtyroká J, Čurda J, Gilíková H, Gürtlerová P, Kabátník P, Kratochvílová H, Manová M, Maštera L, Neudert O, Otava J, Tomanová Petrová P, Šalanský K, Šrámek J, Švecová J, Vít J (2007a) Explanations to Geologic map of the Czech Republic 1:25,000, sheet 24-321 Tišnov. Czech Geological Survey, Prague, pp 1–84

    Google Scholar 

  • Hanžl P, Janoušek V, Žáček V, Wilimský D, Aichler J, Erban V, Pudilová M, Chlupáčová M, Buriánková K, Mixa P, Pecina V (2007b) Magmatic history of granite-derived mylonites from the southern Desná Unit (Silesicum, Czech Republic). Mineral Petrol 89:45–75

    Article  Google Scholar 

  • Heilbron M, Machado N (2003) Timing of terrane accretion in the Neoproterozoic–Eopaleozoic Ribeira orogen (SE Brazil). Precambr Res 125:87–112

    Article  Google Scholar 

  • Hladil J, Melichar R, Otava J, Galle A, Krs M, Man O, Pruner P, Čejchan P, Orel P (1999) The Devonian in the easternmost Variscides, Moravia: a holistic analysis directed towards comprehension of the original context. Abh Geol BA 54:27–47

    Google Scholar 

  • Höck V (1995) Moravian zone: Metamorphic Evolution. In: Dallmeyer RD, Franke W, Weber K (eds) Pre-Permian geology of Central and Eastern Europe. Springer, Berlin, pp 541–553

    Chapter  Google Scholar 

  • Höck V, Montag O, Leichmann J (1997) Ophiolite remnants at the eastern margin of the Bohemian Massif and their bearing on the tectonic evolution. Mineral Petrol 60:267–287

    Article  Google Scholar 

  • Hönig S, Čopjaková R, Škoda R, Novák M, Dolejš D, Leichmann J, Galiová-Vašínová M (2014) Garnet as a major carrier of the Y and REE in the granitic rocks: An example from the layered anorogenic granite in the Brno Batholith, Czech Republic. Am Mineral 99:1922–1941

    Article  Google Scholar 

  • Horn I, Rudnick RL, McDonough WF (2000) Precise elemental and isotope ratio determination by simultaneous solution nebulization and laser ablation-ICP-MS: application to U–Pb geochronology. Chem Geol 164:281–301

    Article  Google Scholar 

  • Irvine TN, Baragar WRA (1971) A guide to the chemical classification of the common volcanic rocks. Can J Earth Sci 8:523–548

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Jacobsen SB, Wasserburg GJ (1980) Sm–Nd isotopic evolution of chondrites. Earth Planet Sci Lett 50:139–155

    Article  Google Scholar 

  • Janoušek V (2006) Saturnin, R language script for application of accessory-mineral saturation models in igneous geochemistry. Geol Carpath 57:131–142

    Google Scholar 

  • Janoušek V, Farrow CM, Erban V (2006) Interpretation of Whole-rock Geochemical Data in Igneous Geochemistry: Introducing Geochemical Data Toolkit (GCDkit). J Petrol 47:1255–1259

    Article  Google Scholar 

  • Janoušek V, Wiegand B, Žák J (2010) Dating the onset of Variscan crustal exhumation in the core of the Bohemian Massif: new U–Pb single zircon ages from the high-K calc-alkaline granodiorites of the Blatná suite, Central Bohemian Plutonic Complex. J Geol Soc Lond 167:347–360

    Article  Google Scholar 

  • Jelínek E, Dudek A (1993) Geochemistry of the subsurface Precambrian plutonic rocks from the Brunovistulian complex in the Bohemian massif, Czechoslovakia. Precambr Res 62:103–125

    Article  Google Scholar 

  • Jensen LS (1976) A new cation plot for classifying Subalkalic Volcanic Rocks. Ont Geol Surv Misc Pap 66:1–22

    Google Scholar 

  • Kalvoda J, Melichar R, Leichmann J, Bábek O (2002) Late Proterozoic–Paleozoic tectonostratigraphic development and paleogeography of Brunovistulian Terrane and comparison with other terranes at the SE margins of Baltica-Laurussia. J Czech Geol Soc 47:3–4

    Google Scholar 

  • Kalvoda J, Bábek O, Fatka O, Leichmann J, Melichar R, Nehyba S, Špaček P (2008) Brunovistulian Terrane (Bohemian Massif, Central Europe) from Late Proterozoic to Late Paleozoic: a review. Int J Earth Sci 97:497–518

    Article  Google Scholar 

  • Kemnitz H, Romer R, Oncken O (2002) Gondwana break-up and the northern margin of the Saxothuringian belt (Variscides of Central Europe). Int J Earth Sci 91:246–259

    Article  Google Scholar 

  • Konopásek J, Schulmann K, Johan V (2002) Eclogite-facies metamorphism at the eastern margin of the Bohemian Massif—subduction prior to continental underthrusting? Eur J Mineral 14:701–713

    Article  Google Scholar 

  • Konopásek J, Sláma J, Košler J (2016) Linking the basement geology along the Africa–South America coasts in the South Atlantic. Precambr Res 280:221–230

    Article  Google Scholar 

  • Košler J, Sylvester PJ (2003) Present trends and the future of zircon in geochronology: laser ablation ICP-MS. In: Hanchar JM, Hoskin PWO (eds) Zircon. Mineralogical Society of America and Geochemical Society Reviews in Mineralogy and Geochemistry 53:243–275

  • Košler J, Fonneland H, Sylvester PJ, Tubrett M, Pedersen RB (2002) U–Pb dating of detrital zircons for sediment provenance studies—a comparison of laser ablation ICP-MS and SIMS techniques. Chem Geol 182:605–618

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Kröner A, Wendt I, Liew TC, Compston W, Todt W, Fiala J, Vaňková V, Vaněk J (1988) U–Pb zircon and Sm–Nd model ages of high-grade Moldanubian metasediments, Bohemian Massif, Czechoslovakia. Contrib Mineral Petrol 99:257–266

    Article  Google Scholar 

  • Kröner A, Štípská P, Schulmann K, Jaeckel P (2000) Chronological constrains on the pre-Variscan evolution of the northeastern margin of the Bohemian Massif, Czech Republic. In: Franke W, Haak V, Oncken O, Tanner D (eds) Orogenic Processes: Quantification and Modelling in the Variscan fold belt. Geological Society, London, Special Publications 179, pp 175–197

  • Kuznetsov NB, Soboleva AA, Udoratina OV, Hertseva MV, Andreichev VL (2007) Pre-Ordovician tectonic evolution and volcano-plutonic associations of the Timanides and northern Pre-Uralides, northeast part of the East European Craton. Gondwana Res 12:05–323

    Article  Google Scholar 

  • Kuznetsov NB, Natapov LM, Belousova EA, O’Reilly SY, Griffin WL (2010) Geochronological, geochemical and isotopic study of detrital zircon suites from Late Neoproterozoic clastic strata along the NE margin of the East European Craton: implications for plate tectonic models. Gondwana Res 17:583–601

    Article  Google Scholar 

  • Leichmann J, Höck V (2008) The Brno Batholith: an insight into the magmatic and metamorphic evolution of the Cadomian Brunovistulian Unit, eastern margin of the Bohemian Massif. J Geosci 53:281–305

    Google Scholar 

  • Liew TC, Hofmann AW (1988) Precambrian crustal components, plutonic associations, plate environment of the Hercynian Fold Belt of central Europe: Indications from a Nd and Sr isotopic study. Contrib Mineral Petrol 98:129–138

    Article  Google Scholar 

  • Linnemann U, Romer RL (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

    Article  Google Scholar 

  • Linnemann U, McNaughton NJ, Romer RL, 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. Int J Earth Sci 93:683–705

    Article  Google Scholar 

  • Linnemann U, Pereira F, Jeffries TE, Drost K, Gerdes A (2008) 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

    Article  Google Scholar 

  • 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). Precambr Res 244:236–278

    Article  Google Scholar 

  • Ludwig KR (2008) User’s Manual for Isoplot v. 3.6, A Geochronological Toolkit for Microsoft Excel. Berkeley Geochronological Center Special Publications 4, pp 1–77

  • Lugmair GW, Marti K (1978) Lunar initial 143Nd/144Nd: differential evolution line of the lunar crust and mantle. Earth Planet Sci Lett 39:349–357

    Article  Google Scholar 

  • Mašek J, Zoubek J (1980) Proposal of stratigraphical terms for stratigraphical units of the Barrandian Proterozoic. Bull Czech Geol Surv 55:121–123

    Google Scholar 

  • Matte P, Maluski H, Rajlich P, Franke W (1990) Terrane boundaries in the Bohemian Massif: result of large-scale Variscan shearing. Tectonophysics 177:151–170

    Article  Google Scholar 

  • Mazur S, Kröner A, Szczepański J, Turniak K, Hanžl P, Melichar R, Rodionov NV, Paderin I, Sergeev SA (2010) Single zircon U–Pb ages and geochemistry of granitoid gneisses from SW Poland: evidence for an Avalonian affinity of the Brunian microcontinent. Geol Mag 147:508–526

    Article  Google Scholar 

  • Mazur S, Szczepański J, Turniak K, McNaughton NJ (2012) Location of the Rheic suture in the eastern Bohemian Massif: evidence from detrital zircon data. Terra Nova 24:199–206

    Article  Google Scholar 

  • McLelland JM, Selleck BW, Bickford ME (2010) Review of the Proterozoic evolution of the Grenville Province, its Adirondack outlier, and the Mesoproterozoic inliers of the Appalachians. In: Tollo RP, Bartholomew MJ, Hibbard, JP, Karabinos PM (eds) From Rodinia to Pangea: the lithotectonic record of the Appalachian region. Geological Society of America, Memoirs 206, pp 21–49

  • Míková J, Denková P (2007) Modified chromatographic separation scheme for Sr and Nd isotope analysis in geological silicate samples. J Geosci 52:221–226

    Google Scholar 

  • Miller CF, McDowell SM, Mapes RW (2003) Hot and cold granites? Implications of zircon saturation temperatures and preservation of inheritance. Geology 31:529–532

    Article  Google Scholar 

  • Moczydlowska M (1997) Proterozoic and Cambrian successions in Upper Silesia: an Avalonian Terrane in southern Poland. Geol Mag 134:679–689

    Article  Google Scholar 

  • Murphy JB, Eguiluz L, Zulauf G (2002) Cadomian orogens, peri-Gondwanan correlatives and Laurentia–Baltica connections. Tectonophysics 352:1–9

    Article  Google Scholar 

  • Murphy JB, Pisarevsky SA, Nance RD, Keppie JD (2004) Neoproterozoic-Early Paleozoic evolution of peri-Gondwanan terranes: implications for Laurentia–Gondwana connections. Int J Earth Sci (Geol Rundsch) 93:659–682

    Article  Google Scholar 

  • 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

    Article  Google Scholar 

  • Nance RD, Linnemann U (2008) The Rheic Ocean: origin, evolution, and significance. GSA Today 18:4–12

    Article  Google Scholar 

  • Nance RD, Murphy JB, Strachan RA, D’Lemos RS, Taylor GK (1991) Late Proterozoic tectonostratigraphic evolution of the Avalonian and Cadomian terranes. Precambr Res 53:41–78

    Article  Google Scholar 

  • Nance RD, Murphy JB, Keppie JD (2002) A Cordilleran model for the evolution of Avalonia. Tectonophysics 352:11–31

    Article  Google Scholar 

  • Nance RD, Gutiérrez-Alonso G, Keppie JD, Linnemann U, Murphy JB, Quesada C, Strachan R, Woodcock NH (2010) Evolution of the Rheic Ocean. Gondwana Res 17:194–222

    Article  Google Scholar 

  • Nawrocki J, Źylińska A, Bula Z, Grabowski J, Krywiec P, Poprawa P (2004) Early Cambrian location and affinities of the Brunovistulian Terrane (Central Europe) in the light of palaeomagnetic data. J Geol Soc Lond 161:513–522

    Article  Google Scholar 

  • Nawrocki J, Dunlap J, Pecskay Z, Krzemiński L, Źylińska A, Fanning M, Kozłowski W, Salwa S, Szczepanik Z, Trela W (2007) Late Neoproterozoic to Early Palaeozoic palaeogeography of the Holy Cross Mountains (Central Europe): an integrated approach. J Geol Soc Lond 164:405–423

    Article  Google Scholar 

  • Neubauer F (2002) Evolution of late Neoproterozoic to early Paleozoic tectonic elements in Central and Southeast European Alpine mountain belts: review and synthesis. Tectonophysics 352:87–103

    Article  Google Scholar 

  • Oberc-Dziedzic T, Klimas K, Kryza R, Fanning CM (2003) SHRIMP zircon geochronology of the Strzelin gneiss, SW Poland: evidence for a Neoproterozoic thermal event in the Fore-Sudetic Block, Central European Variscides. Int J Earth Sci 92:701–711

    Article  Google Scholar 

  • Paterson SR, Ducea MN (2015) Arc Magmatic Tempos: Gathering the Evidence. Elements 11:91–98

    Article  Google Scholar 

  • Paton C, Woodhead JD, Hellstrom JC, Hergt JM, Greig A, Maas R (2010) Improved laser ablation U–Pb zircon geochronology through robust downhole fractionation correction. Geochem Geophys Geosyst. doi:10.1029/2009GC002618

    Google Scholar 

  • Pearce JA, Harris NBW, Tindle AG (1984) Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. J Petrol 25:956–983

    Article  Google Scholar 

  • Pease VL, Dovzhikova E, Beliakova L, Gee DG (2004) Late Neoproterozoic granitoid magmatism in the basement to the Pechora Basin, NW Russia: geochemical constraints indicate westward subduction beneath NE Baltica. In: Gee DG (ed) The Neoproterozoic Timanide Orogen of Eastern Baltica. Geological Society, London, Memoirs 30:75–85

  • Peccerillo A, Taylor SR (1976) Geochemistry of Eocene calc-alkaline volcanic rocks from the Kastamonu area, Northern Turkey. Contrib Mineral Petrol 58:63–81

    Article  Google Scholar 

  • Pereira MF, Chichorro M, Solá AR, Silva JB, Sánchez-García T, Bellido F (2011) Tracing the Cadomian magmatism with detrital/inherited zircon ages by in situ U–Pb SHRIMP geochronology (Ossa-Morena Zone, SW Iberian Massif). Lithos 123:204–217

    Article  Google Scholar 

  • Petrus JA, Kamber BS (2012) VizualAge: A Novel Approach to Laser Ablation ICP-MS U–Pb Geochronology Data Reduction. Geostand Geoanal Res 36:247–270

    Article  Google Scholar 

  • Pin C, Zalduegui JFS (1997) Sequential separation of light rare-earth elements, thorium and uranium by miniaturized extraction chromatography: application to isotopic analyses of silicate rocks. Anal Chim Acta 339:79–89

    Article  Google Scholar 

  • Pin C, Briot D, Bassin C, Poitrasson F (1994) Concomitant separation of strontium and samarium–neodymium for isotopic analysis in silicate samples, based on specific extraction chromatography. Anal Chim Acta 298:209–217

    Article  Google Scholar 

  • Romano SS, Dörr W, Zulauf G (2004) Cambrian granitoids in pre-Alpine basement of Crete (Greece): evidence from U–Pb dating of zircon. Int J Earth Sci 93:844–859

    Article  Google Scholar 

  • Rubio-Ordóñez A, Gutiérrez-Alonso G, Valverde-Vaquero P, Cuesta A, Gallastegui G, Gerdes A, Cárdenes V (2015) Arc-related Ediacaran magmatism along the northern margin of Gondwana: geochronology and isotopic geochemistry from Northern Iberia. Gondwana Res 27:216–227

    Article  Google Scholar 

  • Şahin SY, Aysal N, Güngör Y, Peytcheva I, Neubauer F (2014) Geochemistry and U–Pb zircon geochronology of metagranites in Istranca (Strandja) Zone, NW Pontides, Turkey: implications for the geodynamic evolution of Cadomian Orogeny. Gondwana Res 26:755–771

    Article  Google Scholar 

  • Samson SD, D’Lemos RS, Miller BV, Hamilton MA (2005) Neoproterozoic palaeogeography of the Cadomia and Avalon terranes: constraints from detrital zircon U–Pb ages. J Geol Soc Lond 162:65–71

    Article  Google Scholar 

  • Schaltegger U, Nägler TF, Corfu F, Maggetti M, Galetti G, Stosch H (1997) A Cambrian island arc in the Silvretta nappe: constraints from geochemistry and geochronology. Schweiz Mineral Petrogr Mitt 77:337–350

    Google Scholar 

  • Schaltegger U, Schmitt AK, Horstwood MSA (2015) U–Th–Pb zircon geochronology by ID-TIMS, SIMS, and laser ablation ICP-MS: Recipes, interpretations, and opportunities. Chem Geol 402:89–110

    Article  Google Scholar 

  • Scharbert S, Batík P (1980) The age of the Thaya (Dyje) Pluton. Verh Geol Bundesanst 1980:325–331

    Google Scholar 

  • Schulmann K, Ledru P, Autran A, Melka R, Lardeaux JM, Urban M, Lobkowicz M (1991) Evolution of nappes in the eastern margin of the Bohemian Massif: a kinematic interpretation. Geol Rundsch 80:73–92

    Article  Google Scholar 

  • Schulmann K, Melka R, Lobkowicz MZ, Ledru P, Lardeaux JM, Autran A (1994) Contrasting styles of deformation during progressive nappe stacking at the southeastern margin of the Bohemian Massif (Thaya Dome). J Struct Geol 16:355–370

    Article  Google Scholar 

  • Schulmann K, Konopásek J, Janoušek V, Lexa O, Lardeaux JM, Edel JB, Štípská P, Ulrich S (2009) An Andean type Palaeozoic convergence in the Bohemian Massif. Comptes Rendus Geosci 341:266–286

    Article  Google Scholar 

  • Schulmann K, Lexa O, Janoušek V, Lardeaux JM, Edel JB (2014) Anatomy of a diffuse cryptic suture zone: an example from the Bohemian Massif, European Variscides. Geology 42:275–278

    Article  Google Scholar 

  • Schulz B, Bombach K, Pawlig S, Brätz H (2004) Neoproterozoic to Early-Palaeozoic magmatic evolution in the Gondwana-derived Austroalpine basement to the south of the Tauern Window (Eastern Alps). Int J Earth Sci 93:824–843

    Article  Google Scholar 

  • Shafaii Moghadam H, Khademi M, Hu Z, Stern RJ, Santos JF, Wu Y (2015) Cadomian (Ediacaran–Cambrian) arc magmatism in the ChahJam–Biarjmand Metamorphic Complex (Iran): magmatism along the northern active margin of Gondwana. Gondwana Res 27:439–452

    Article  Google Scholar 

  • Sláma J, Dunkley DJ, Kachlík V, Kusiak MA (2008a) Transition from island-arc to passive setting on the continental margin of Gondwana: U–Pb zircon dating of Neoproterozoic metaconglomerates from the SE margin of the Teplá–Barrandian Unit, Bohemian Massif. Tectonophysics 461:44–59

    Article  Google Scholar 

  • Sláma J, Košler J, Condon DJ, Crowley JL, Gerdes A, Hanchar JM, Horstwood MSA, Morris GA, Nasdala L, Norberg N, Schaltegger U, Schoene B, Tubrett MN, Whitehouse MJ (2008b) Plešovice zircon—a new natural reference material for U–Pb and Hf isotopic microanalysis. Chem Geol 249:1–35

    Article  Google Scholar 

  • Soejono I, Žáčková E, Janoušek V, Machek M, Košler J (2010) Vestige of an Early Cambrian incipient oceanic crust incorporated in the Variscan orogen: Letovice Complex, Bohemian Massif. J Geol Soc Lond 167:1113–1130

    Article  Google Scholar 

  • Souček J, Jelínek E, Bowes DR (1992) Geochemistry of gneisses of the eastern margin of the Bohemian Massif. In: Kukal Z (ed) Proceedings of the 1st international conference on the Bohemian Massif. Czech Geological Survey, Prague, pp 269–285

    Google Scholar 

  • Steiger RH, Jäger E (1977) Subcommission on geochronology: convention on the use of decay constants in geo- and cosmochronology. Earth Planet Sci Lett 36:359–362

    Article  Google Scholar 

  • Štípská P, Schulmann K (1995) Inverted metamorphic zonation in a basement-derived nappe sequence, eastern margin of the Bohemian Massif. Geol J 30:385–413

    Article  Google Scholar 

  • Štípská P, Hacker BR, Racek M, Holder R, Kylander-Clark ARC, Schulmann K, Hasalová P (2015) Monazite dating of prograde and retrograde P–T–d paths in the Barrovian terrane of the Thaya Window, Bohemian Massif. J Petrol 56:1007–1035

    Article  Google Scholar 

  • Strachan RA, D’Lemos RS, Dallmeyer RD (1996) Late Precambrian evolution of an active plate margin: North Armorican Massif, France. In: Nance RD, Thompson MD (eds) Avalonian and related Peri-Gondwanan terranes of the Circum–North Atlantic. Geological Society of America, Special Papers 304, pp 319–332

  • Strnad L, Mihaljevič M (2005) Sedimentary provenance of Mid-Devonian clastic sediments in the Teplá–Barrandian Unit (Bohemian Massif): U–Pb and Pb–Pb geochronology of detrital zircons by laser ablation ICP-MS. Mineral Petrol 84:47–68

    Article  Google Scholar 

  • Suess FE (1912) Die moravische Fenster und ihre Beziehung zum Grundgebirge des Hohen Gesenkes. Denkschr Österr Akad Wiss Mat Naturwiss Kl 88:541–631

    Google Scholar 

  • Suess FE (1926) Intrusionstektonik und Wandertektonik im variszischen Grundgebirge. Verlag von Gebrüder Borntraeger, Berlin, pp 1–268

    Google Scholar 

  • Tait JA, 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 

  • Taylor SR, McLennan SM (1995) The geochemical evolution of the continental crust. Rev Geophys 33:241–265

    Article  Google Scholar 

  • Tedeschi M, Novo T, Pedrosa-Soares A, Dissin I, Tassinari C, Silva LC, Gonçalves L, Alkmim F, Lana C, Figueiredo C, Dantes E, Medeiros S, De Campos C, Corrales F, Heilbron M (2016) The Ediacaran Rio Doce arc revisited (Araçuaí–Ribeira orogenic system, SE Brazil). J South Am Earth Sci 68:167–186

    Article  Google Scholar 

  • Ustaömer PA, Mundil R, Renne PR (2005) U/Pb and Pb/Pb zircon ages for arc-related intrusions of the Bolu Massif (W Pontides, NW Turkey): evidence for Late Precambrian (Cadomian) age. Terra Nova 17:215–223

    Article  Google Scholar 

  • Valverde-Vaquero P, Dörr W, Belka Z, Franke W, Wiszniewska J, Schastok J (2000) U–Pb single-grain dating of detrital zircon in the Cambrian of Central Poland: implications for Gondwana versus Baltica provenance studies. Earth Planet Sci Lett 184:225–240

    Article  Google Scholar 

  • van Breemen O, Aftalion M, Bowes DR, Dudek A, Mísař Z, Povondra P, Vrána S (1982) Geochronological studies of the Bohemian Massif, Czechoslovakia, and their significance in the evolution of Central Europe. Trans R Soc Edinb Earth Sci 73:89–108

    Article  Google Scholar 

  • Vavrdová M, Mikuláš R, Nehyba S (2003) Lower Cambrian siliciclastic sediments in southern Moravia (Czech Republic) and their paleogeographical constraints. Geol Carpath 54:67–79

    Google Scholar 

  • Villaseca C, Barbero L, Herreros V (1998) A re-examination of the typology of peraluminous granite types in intracontinental orogenic belts. Trans R Soc Edinb Earth Sci 89:113–119

    Article  Google Scholar 

  • von Raumer JF, Stampfli GM (2008) The birth of the Rheic Ocean—Early Palaeozoic subsidence patterns and subsequent tectonic plate scenarios. Tectonophysics 461:9–20

    Article  Google Scholar 

  • von Raumer JF, Stampfli GM, Borel G, Bussy F (2002) Organization of pre-Variscan basement areas at the north-Gondwanan margin. Int J Earth Sci 91:35–52

    Article  Google Scholar 

  • Wasserburg GJ, Jacobsen SB, DePaolo DJ, McCulloch MT, Wen T (1981) Precise determination of Sm/Nd ratios, Sm and Nd isotopic abundances in standard solutions. Geochim Cosmochim Acta 45:2311–2324

    Article  Google Scholar 

  • Watson EB, Harrison TM (1983) Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types. Earth Planet Sci Lett 64:295–304

    Article  Google Scholar 

  • 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 Rundsch 82:42–50

    Article  Google Scholar 

  • Wiedenbeck M, Allé P, Corfu F, Griffin WL, Meier M, Oberli F, von Quadt A, Roddick JC, Spiegel W (1995) Three natural zircon standards for U–Th–Pb, Lu–Hf, trace element and REE analyses. Geostand Newsl 19:1–23

    Article  Google Scholar 

  • Winchester J, Pharaoh T, 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, London, Special Publications 201, pp 1–18

  • Winchester JA, Pharaoh TC, Verniers J, Ioane D, Seghedi A (2006) Palaeozoic accretion of Gondwana-derived terranes to the East European Craton: recognition of detached terrane fragments dispersed after collision with promontories. In: Gee DG, Stephenson RA (eds) European Lithosphere Dynamics. Geological Society London, Memoirs 32, pp 323–332

  • Wood DA (1980) The application of a Th–Hf–Ta diagram to problems of tectonomagmatic 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

    Article  Google Scholar 

  • Žák J, Kraft P, Hajná J (2013) Timing, styles, and kinematics of Cambro–Ordovician extension in the Teplá–Barrandian Unit, Bohemian Massif, and its bearing on the opening of the Rheic Ocean. Int J Earth Sci 102:415–433

    Article  Google Scholar 

  • Zulauf G, Dörr W, Fiala J, Vejnar Z, 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 Rundsch 86:571–584

    Article  Google Scholar 

Download references

Acknowledgements

We are indebted to F. Veselovský for separation of zircons, V. Erban for Sr–Nd isotopic analyses, M. Racek for CL imaging and S. Vrána for helpful discussions. We also thank A. Gerdes for editorial handling of this manuscript. The manuscript benefited from constructive reviews by G. Zulauf and one anonymous colleague. This study was supported by the Czech Science Foundation (GACR 13-16315S to P. Štípská), by LK11202 programme of the Ministry of Education of the Czech Republic (to K. Schulmann) and partly also by the Academy of Sciences of the Czech Republic institutional support to the Institute of Geophysics of the CAS, v.v.i. (RVO 67985530).

Author information

Authors and Affiliations

  1. Czech Geological Survey, Klárov 3, 118 21, Prague 1, Czech Republic

    Igor Soejono, Vojtěch Janoušek, Eliška Žáčková, Jiří Konopásek & Pavel Hanžl

  2. Institute of Petrology and Structural Geology, Faculty of Science, Charles University, Albertov 6, 128 43, Prague 2, Czech Republic

    Vojtěch Janoušek

  3. Institute of Geology of the CAS, v. v. i., Rozvojová 269, 165 00, Prague 6, Czech Republic

    Jiří Sláma

  4. Department of Geosciences, University of Tromsø – The Arctic University of Norway, Postboks 6050, 9037, Langnes, Tromsø, Norway

    Jiří Konopásek

  5. Institute of Geophysics of the CAS, v. v. i., Boční II-1401, 141 31, Prague 4, Czech Republic

    Matěj Machek

Authors
  1. Igor Soejono
    View author publications

    You can also search for this author in PubMed Google Scholar

  2. Vojtěch Janoušek
    View author publications

    You can also search for this author in PubMed Google Scholar

  3. Eliška Žáčková
    View author publications

    You can also search for this author in PubMed Google Scholar

  4. Jiří Sláma
    View author publications

    You can also search for this author in PubMed Google Scholar

  5. Jiří Konopásek
    View author publications

    You can also search for this author in PubMed Google Scholar

  6. Matěj Machek
    View author publications

    You can also search for this author in PubMed Google Scholar

  7. Pavel Hanžl
    View author publications

    You can also search for this author in PubMed Google Scholar

Corresponding author

Correspondence to Igor Soejono.

Electronic supplementary material

Below is the link to the electronic supplementary material.

Laser ablation ICP-MS U–Pb zircon data (PDF 226 kb)

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Soejono, I., Janoušek, V., Žáčková, E. et al. Long-lasting Cadomian magmatic activity along an active northern Gondwana margin: U–Pb zircon and Sr–Nd isotopic evidence from the Brunovistulian Domain, eastern Bohemian Massif. Int J Earth Sci (Geol Rundsch) 106, 2109–2129 (2017). https://doi.org/10.1007/s00531-016-1416-y

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s00531-016-1416-y

Keywords

Search

Navigation