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Author's personal copyK. Schulmann et al. / C. R. Geoscience 341 (2009) 266–286 283[52] V. Havlíček, J. Vaněk, O. Fatka, Perunica microcontinent in theOrdovician (its position within the Mediterranean Province,series division, benthic and pelagic associations), Sb. Geologick.Ved Paleontol. 46 (1994) 23–56.[53] F. Holub, Ultrapotassic plutonic rocks of the durbachite seriesin the Bohemian Massif: petrology, geochemistry and petrogeneticinterpretation, J. Geol. Sci. Econ. Geol. Min. 31 (1997)5–26.[54] F. Holub, M. Klečka, D. Matějka, Moldanubian Zone VII. C. 3.Igneous activity, in : R. Dallmeyer, W. Franke, K. Weber (Eds.),Pre-Permian Geology of central and eastern Europe, Springer,Berlin, 1995, pp. 444–452.[55] F. Holub, A. Cocherie, P. Rossi, Radiometric dating of graniticrocks from the Central Bohemian Plutonic Complex (CzechRepublic): constraints on the chronology of thermal and tectonicevents along the Moldanubian-Barrandian boundary, C. R.Acad. Sci. Ser. IIa 325 (1997) 19–26.[56] F. Holub, J. Machart, M. Manová, The Central BohemianPlutonic Complex: geology, chemical composition and geneticinterpretation, J. Geol. Sci. Econ. Geol. Min. 31 (1997) 27–50.[57] F. Hrouda, O. Krejčí, J. Otava, Magnetic fabric in folds of theeasternmost Rheno-Hercynian Zone, Phys. Chem. Earth Part A.25 (2000) 505–510.[58] F. Hrouda, Š. Taborská, K. Schulmann, J. Ježek, D. Dolejš,Magnetic fabric and rheology of co-mingled magmas in theNasavrky Plutonic Complex (E Bohemia); implications forintrusive strain regime and emplacement mechanism, Tectonophysics30 (1999) 93–111.[59] V. Janoušek, F. Holub, The causal link between HP/HT metamorphismand ultrapotassic magmatism in collisional orogens:case study from the Moldanubian Zone of the BohemianMassif, Proc. Geol. Assoc. 118 (2007) 75–86.[60] V. Janoušek, G. Rogers, D. Bowes, Sr-Nd isotopic constraintson the petrogenesis of the Central Bohemian Pluton, CzechRepublic, Int. J. Earth Sci. 84 (1995) 520–534.[61] V. Janoušek, D.R. Bowes, C.J.R. Braithwaite, G. Rogers,Microstructural and mineralogical evidence for limited involvementof magma mixing in the petrogenesis of a Hercynianhigh-K calc-alkaline intrusion: the Kozárovice granodiorite,Central Bohemian Pluton, Czech Republic, Trans. R. Soc.Edinburgh Earth Sci. 91 (2000) 15–26.[62] V. Janoušek, D.R. Bowes, G. Rogers, C.M. Farrow, E. Jelínek,Modelling diverse processes in the petrogenesis of a compositebatholith: the Central Bohemian Pluton, Central EuropeanHercynides, J. Petrol. 41 (2000) 511–543.[63] V. Janoušek, F. Holub, A. Gerdes, K-rich magmatism in theMoldanubian Unit, Bohemian Massif – a complex story featuringvariably enriched lithospheric mantle melts and theirinteraction with the crust, Geolines 16 (2003) 48–49.[64] V. Janoušek, C. Braithwaite, D. Bowes, A. Gerdes, Magmamixingin the genesis of Hercynian calc-alkaline granitoids: anintegrated petrographic and geochemical study of the Sázavaintrusion, Central Bohemian Pluton, Czech Republic, Lithos 78(2004) 67–99.[65] V. Janoušek, S. Vrána, V. Erban, K. Vokurka, M. Drábek,Metabasic rocks in the Varied Group of the Moldanubian Zone,southern Bohemia – their petrology, geochemical character andpossible petrogenesis, J. Geosci. 53 (2008) 31–64.[66] V. Janoušek, F. Finger, M. Roberts, J. Frýda, C. Pin, D. Dolejš,Deciphering the petrogenesis of deeply buried granites: wholerockgeochemical constraints on the origin of largely undepletedfelsic granulites from the Moldanubian Zone of theBohemian Massif, Trans. R. Soc. Edinburgh: Earth Sci. 95(2004) 141–159.[67] V. Janoušek, A. Gerdes, S. Vrána, F. Finger, V. Erban, G. Friedl,C.J.R. Braithwaite, Low-pressure granulites of the Lišov Massif,southern Bohemia: Visean metamorphism of Late Devonianplutonic arc rocks, J. Petrol. 47 (2006) 705–744.[68] J. Kalvoda, O. Bábek, O. Fatka, J. Leichmann, R. Melichar, S.Nehyba, P. Špaček, Brunovistulian terrane (Bohemian Massif,central Europe) from Late Proterozoic to late Paleozoic: areview, Int. J. Earth Sci. 97 (2008) 497–518.[69] H. Klápová, J. Konopásek, K. Schulmann, Eclogites from theCzech part of the Erzgebirge multi-stage metamorphic andstructural evolution, J. Geol. Soc. 155 (1998) 567–583.[70] J. Konopásek, K. Schulmann, Variscan transpressional deformationand crustal folding in the Krkonose Mountains (northernmargin of the Bohemian Massif), in : K. Schulmann (Ed.),Palaeozoic orogenesis and crustal evolution of European lithosphere,Univerzita Karlova, Prague, Czech Republic, 1998, pp.279–280.[71] J. Konopásek, K. Schulmann, Contrasting Early Carboniferousfield geotherms: evidence for accretion of a thickened orogenicroot and subducted Saxothuringian crust (central EuropeanVariscides), J. Geol. Soc. 162 (2005) 463–470.[72] J. Konopásek, K. Schulmann, O. Lexa, Structural evolution ofthe central part of the Krusne hory (Erzgebirge) Mountains inthe Czech Republic - evidence for changing stress regimeduring Variscan compression, J. Struct. Geol. 23 (2001) 1373–1392.[73] J. Konopásek, K. Schulmann, V. Johan, Eclogite-facies metamorphismat the eastern margin of the Bohemian Massif –subduction prior to continental underthrusting? Eur. J. Mineral.14 (2002) 701–713.[74] J. Košler, M. Aftalion, D. Bowes, Mid–Late Devonian plutonicactivity in the Bohemian Massif: U–Pb zircon isotopic evidencefrom the Staré Sedlo and Mirotice gneiss complexes, CzechRepublic, Neues Jahrb. Miner. Monat. (1993) 417–431.[75] J. Košler, S. Kelley, D. Vance, M. Svojtka, Independent datingof cooling and decompression of high grade rocks in theSouthern Bohemian Massif with Ar-Ar, Sm-Nd and U-PbTechniques, J. Conf. Abs. 4 (1999) 39.[76] J. Košler, D.R. Bowes, J. Konopásek, J. Míková, Laser ablationICPMS dating of zircons in Erzgebirge orthogneisses: evidencefor Early Cambrian and Early Ordovician granitic plutonism inthe western Bohemian Massif, Eur. J. Mineral. 16 (2004) 15–22.[77] M. Košuličová, P. Špaček, Variations in the transient progradegeothermal gradient from chloritoid-staurolite equilibria: a casestudy from the Barrovian and Buchan-type domains in theBohemian Massif, J. Metamorph. Geol. 25 (2007) 19–36.[78] M. Košuličová, R. Montigny, K. Schulmann, P. Špaček, LatePaleozoic thermal overprints exemplified by Th-U-Pb monaziteand K-Ar mica dating at the eastern margin of the BohemianMassif (West Sudets, Czech Republic), Bull. Soc. geol. France(2008), submitted for publication.[79] J. Kotková, Tectonometamorphic history of lower crust in theBohemian Massif: example of north Bohemian granulites,Czech Geol. Surv. Spec. Paper 2 (1993) 1–42.[80] J. Kotková, A. Kröner, W. Todt, J. Fiala, Zircon dating of NorthBohemian granulites, Czech Republic: further evidence for theLower Carboniferous high-pressure event in the BohemianMassif, Geol. Rundsch. 85 (1996) 154–161.[81] J. Kotková, A. Gerdes, R. Parrish, M. Novák, Clasts of Variscanhigh-grade rocks within Upper Visean conglomerates-cons-176
Author's personal copy284K. Schulmann et al. / C. R. Geoscience 341 (2009) 266–286traints on exhumation history from petrology and U-Pb chronology,J. Metamorph. Geol. 25 (2007) 781–801.[82] B. Kříbek, Z. Pouba, V. Skoček, J. Waldhausrová, Neoproterozoicof the Teplá-Barrandian Unit as a part of the Cadomianorogenic belt: a review and correlation aspects, Bull. CzechGeol. Soc. 75 (2000) 175–196.[83] A. Kröner, A. Willner, Time of formation and peak of VariscanHP-HT metamorphism of quartz-feldspar rocks in the centralErzgebirge, Saxony, Germany, Contrib. Mineral. Petrol. 132(1998) 1–20.[84] A. Kröner, P. O’Brien, A. Nemchin, R. Pidgeon, Zircon agesfor high pressure granulites from South Bohemia, CzechRepublic, and their connection to Carboniferous high temperatureprocesses, Contrib. Mineral. Petrol. 138 (2000) 127–142.[85] A. Kröner, A. Willner, E. Hegner, A. Frischbutter, J. Hofmann,R. Bergner, Latest Precambrian (Cadomian) zircon ages, Ndisotopic systematics and PT evolution of granitoid orthogneissesof the Erzgebirge, Saxony and Czech Republic, Int. J. EarthSci. 84 (1995) 437–456.[86] M. Krs, P. Pruner, Paleomagnetism, Palaeogeography of theVariscan Formations of the Bohemian Massif, J. Czech. Geol.Soc. 40 (1995) 3–45.[87] S. Lamb, L. Hoke, L. Kennan, J. Dewey, Cenozoic evolution ofthe central Andes in Bolivia and northern Chile, Geol. Soc.London Spec. Publ. 121 (1997) 237–264.[88] T. Liew, F. Finger, V. Höck, The Moldanubian granitoid plutonsof Austria: chemical and isotopic studies bearing on theirenvironmental setting, Chem. Geol. 76 (1989) 41–55.[89] U. Linnemann, N.J. McNaughton, R.L. Romer, M. Gehmlich,K. Drost, C. Tonk, West African provenance for Saxo-Thuringia(Bohemian Massif): did Armorica ever leave pre-PangeanGondwana? U/Pb-SHRIMP zircon evidence and the Nd-isotopicrecord, Int. J. Earth Sci. 93 (2004) 683–705.[90] H. Maluski, F. Patočka, Geochemistry and 40 Ar/ 39 Ar geochronologyof the mafic metavolcanic rocks from the RýchoryMountains complex (West Sudetes, Bohemian Massif): palaeotectonicsignificance, Geol. Mag. 134 (1997) 703–716.[91] H. Maluski, P. Rajlich, J. Souček, Pre-Variscan, Variscan andearly Alpine thermo-tectonic history of the north-eastern BohemianMassif; an (super 40) Ar/ (super 39) Ar study, Geol.Rundsch. 84 (1995) 345–358.[92] H.J. Massonne, Early metamorphic evolution and exhumationof felsic high-pressure granulites from the north-western BohemianMassif, Springer Wien, 2006, pp. 177–202.[93] P. Matte, The Variscan collage and orogeny (480–290 Ma) andthe tectonic definition of the Armorica microplate: a review,Terra Nova 13 (2001) 122–128.[94] P. Matte, H. Maluski, P. Rajlich, W. Franke, Terrane boundariesin the Bohemian Massif – result of large-scale Variscan shearing,Tectonophysics 177 (1990) 151.[95] S. Mazur, P. Aleksandrowski, R. Kryza, T. Oberc-Dziedzic, TheVariscan Orogen in Poland, Geol. Q. 50 (2006) 89–118.[96] W.S. McKerrow, C. Mac Niocaill, P.E. Ahlberg, G. Clayton,C.J. Cleal, R.M.C. Eagar, The Late Palaeozoic relations betweenGondwana and Laurussia, Geol. Soc. London Spec. Publ.179 (2000) 9–20.[97] G. Medaris, E. Jelínek, Z. Mísař, Czech eclogites. Terranesettings, interpretation for Variscan tectonic evolution of theBohemian Massif, Eur. J. Mineral. 7 (1995) 7–28.[98] J. Nawrocki, The Devonian–Carboniferous platform paleomagneticdirections from the Silesian–Krakow area and theirimportance for Variscan paleotectonic reconstructions, Geol.Q. 37 (1993) 397–430.[99] P. O’Brien, Garnet zoning and reaction textures in overprintedeclogites, Bohemian Massif, European Variscides: a record oftheir thermal history during exhumation, Lithos 41 (1997) 119–133.[100] P. O’Brien, The fundamental Variscan problem: high-temperaturemetamorphism at different depths and high-pressuremetamorphism at different temperatures, in: W. Franke,V. Haak, O. Oncken, D. Tanner (Eds.), Orogenic Processes:Quantification and Modelling in the Variscan Belt, GeologicalSociety, London, 2000, pp. 369.[101] P. O’Brien, C. Rohr, M. Okrush, M. Patzak, Eclogite faciesrelics and a multistage breakdown in metabasites of the KTBpilot hole, NE Bavaria: implications for the Variscan tectonometamorphicevolution of the NW Bohemian Massif, Contrib.Mineral. Petrol. 112 (1992) 261–278.[102] P.J. O’Brien, D.A. Carswell, Tectonometamorphic evolution ofthe Bohemian Massif - evidence from high-pressure metamorphicrocks, Geol. Rundsch. 82 (1993) 531–555.[103] P.J. O’Brien, S. Vrána, Eclogites with a short-lived granulitefaciesoverprint in the Moldanubian Zone, Czech Republic –petrology, geochemistry and diffusion modeling of garnetzoning, Geol. Rundsch. 84 (1995) 473–488.[104] O. Oncken, C. von Winterfeld, U. Dittmar, Accretion of a riftedpassive margin: the Late Paleozoic Rhenohercynian fold andthrust belt (Middle European Variscides), Tectonics 18 (1999)75–91.[105] O. Oncken, D. Hindle, J. Kley, K. Elger, P. Victor, K. Schemmann,Deformation of the central Andean Upper Plate System—-facts, fiction, and constraints for plateau models, in : O. Oncken,et al. (Eds.), The Andes, Springer Verlag, 2006, pp. 3–27.[106] F. Paris, Early Palaezoic palaeography of northern Gondwanaregions, Acta Univ. Carol. Geol. 42 (1998) 473–483.[107] F. Patočka, J. Valenta, Geochemistry of the Late Devonianintermediate to acid metavolcanic rocks from the southern partof the Vrbno Group, the Jeseniky Mts. (Moravo-Silesian Belt,Bohemian Massif, Czech Republic): paleotectonic implications,Geolines 4 (1996) 42–54.[108] F. Patočka, P. Vlašímský, K. Blechová, Geochemistry of EarlyPaleozoic volcanics of the Barrandian Basin (Bohemian Massif,Czech Republic): implications for Paleotectonic reconstructions,Jahrb. Geol. Bundelsansalt 136 (1993) 871–894.[109] K. Petrakakis, Evolution of Moldanubian rocks in Austria:review and synthesis, J. Metamorph. Geol. 15 (1997) 203–222.[110] P. Pitra, J.P. Burg, M. Giraud, Late-Variscan strike-slip tectonicsbetween the Teplá-Barrandian and Moldanubian terranes(Czech Bohemian Massif): petrostructural evidence, J. Geol.Soc. 156 (1999) 1003–1020.[111] P. Pitra, J.P. Burg, K. Schulmann, P. Ledru, Late Orogenicextension in the Bohemian Massif – petrostructural evidence inthe Hlinsko Region, Geodin. Acta 7 (1994) 15–30.[112] M. Racek, P. Štípská, P. Pitra, K. Schulmann, O. Lexa, Metamorphicrecord of burial and exhumation of orogenic lower andmiddle crust: a new tectonothermal model for the Drosendorfwindow (Bohemian Massif, Austria), Mineral. Petrol. 86(2006) 221–251.[113] P. Rajlich, J. Synek, M. Sarbach, K. Schulmann, Hercynianthrustrelated shear zones and deformation of the Varied Groupon the contact of granulites/southern Moldanubian, BohemianMassif, Int. J. Earth Sci. 75 (1986) 665–683.177
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“It strikes me that all our knowl
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Contentsviii4.7 Schulmann, Konopás
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Dedicated to my wife Markéta, daug
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Foreword 2First topic “Quantitati
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Foreword 4source and freely availab
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1. Quantitative analysis of deforma
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Chapter 2Mechanisms of lower crusta
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2. Mechanisms of lower crustal flow
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Chapter 3Quantitative analyses ofme
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3. Quantitative analyses of metamor
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Bibliography 42Culshaw, N., Beaumon
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Bibliography 44sources and trigger
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Bibliography 46Skrzypek, E., Štíp
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Table 1Statistical values of the qu
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CONTRASTING TEXTURAL RECORD OF TWO
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TEXTURES OF NATURALLY DEFORMED META
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' ~'-----2~--~----TEXTURES OF NATUR
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ClickHereforFullArticleJOURNAL OF G
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B10406SCHULMANN ET AL.: RHEOLOGY OF
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ORIGIN OF FELSIC MIGMATITES 31Ó 20
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ORIGIN OF FELSIC MIGMATITES 33durin
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ORIGIN OF FELSIC MIGMATITES 35(a)Ty
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ORIGIN OF FELSIC MIGMATITES 37(a)Pl
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ORIGIN OF FELSIC MIGMATITES 39Grain
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ORIGIN OF FELSIC MIGMATITES 41(a)(b
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ORIGIN OF FELSIC MIGMATITES 43(a)(b
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ORIGIN OF FELSIC MIGMATITES 45Fig.
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ORIGIN OF FELSIC MIGMATITES 47produ
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ORIGIN OF FELSIC MIGMATITES 49stron
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ORIGIN OF FELSIC MIGMATITES 51Cmı
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ORIGIN OF FELSIC MIGMATITES 53easte
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