296 K. SCHULMANN ET AL.thermal <strong>and</strong> tectonic events along the Moldanubian-Barr<strong>and</strong>ianboundary. Comptes Rendus de lÕAcademie de Sciences –Serie IIa: Sciences de la Terre et des Planetes, 325, 19–26.Jamieson, R. A., Beaumont, C., Nguyen, M. H. & Lee, B., 2002.Interaction <strong>of</strong> metamorphism, deformation <strong>and</strong> exhumation inlarge convergent orogens. Journal <strong>of</strong> Metamorphic Geology,20, 9–24.Jamieson, R. A., Beaumont, C., Medvedev, S. & Nguyen, M. H.,2004. Crustal channel flows: 2. Numerical models withimplications for metamorphism in the Himalayan–Tibetanorogen. Journal <strong>of</strong> Geophysical Research B: Solid Earth, 109,B06407, 1–24.Janousˇek, V. & Holub, F. V., 2007. The causal link between HP–HT metamorphism <strong>and</strong> ultrapotassic magmatism in collisionalorogens: case study from the Moldanubian Zone <strong>of</strong> theBohemian Massif. Proceedings <strong>of</strong> the Geologists Association,118, 75–86.Jastrzębski, M., 2005. The tectonometamorphic evolution <strong>of</strong> themarbles in the Lądek–S´ niez_ nik Metamorphic Unit, WestSudetes. Geologica Sudetica, 37, 1–26.Jezˇek, J., Schulmann, K. & Thompson, A. B., 1998. Modelling <strong>of</strong>strain partitioning in transpression zones. In: Proceedings <strong>of</strong>the Fourth Annual Conference <strong>of</strong> the International Associationfor Mathematical Geology (eds Buccianti, A., Nardi, G. &Potenza, R.), pp. 827–832. De Frede, Naples.Kisters, A. F. M., Charlesworth, E. G., Gibson, R. L. &Anhaeusser, C. R., 1996. Steep structure formation in theOkiep copper district, South Africa: bulk inhomogeneousshortening <strong>of</strong> a high-grade metamorphic granite–gneisssequence. Journal <strong>of</strong> Structural Geology, 18, 735–751.Klemd, R. & Bro¨ cker, M., 1999. Fluid influence on mineralreactions in ultrahigh-pressure granulites: a case study in theSnieznik Mts (West Sudetes, Pol<strong>and</strong>). Contributions to Mineralogy<strong>and</strong> Petrology, 136, 358–373.Kolenovska´ , E., Schulmann, K., Kla´ pova´ , H. & Sˇtı´ pska´ , P.,1999. Tectonometamorphic evolution <strong>of</strong> the Moldanubianzone near Jemnice (south Moravia, Bohemian Massif).Beihefte zum European Journal <strong>of</strong> Mineralogy, 11, 91–110.Konopa´ sek, J. & Schulmann, K., 2005. Contrasting Early Carboniferousfield geotherms: evidence for accretion <strong>of</strong> a thickenedorogenic root <strong>and</strong> subducted Saxothuringian crust(Central European Variscides). Journal <strong>of</strong> the GeologicalSociety, 162, 463–470.Konopa´ sek, J., Schulmann, K. & Johan, V., 2002. Eclogite-faciesmetamorphism at the eastern margin <strong>of</strong> the Bohemian Massif– subduction prior to continental underthrusting? EuropeanJournal <strong>of</strong> Mineralogy, 14, 701–713.Kotkova´ , J., Gerdes, A., Parrish, R.R. & Nova´ k, M., 2007.Clasts <strong>of</strong> Variscan high-grade rocks within Upper Vise´ anconglomerates – constraints on exhumation history frompetrology <strong>and</strong> U–Pb chronology. Journal <strong>of</strong> MetamorphicGeology, 25, 781–801.Kro¨ ner, A., Sˇtı´ pska´ , P., Schulmann, K. & Jaeckel, P., 2000.Geochronological constraints on the pre-Variscan evolution <strong>of</strong>the northeastern margin <strong>of</strong> the Bohemian Massif, CzechRepublic. In: Quantification <strong>and</strong> Modelling in the VariscanBelt, Special Publication 179 (eds Franke, W.H.V., Oncken, O.& Tanner, D.), pp. 175–197. Geological Society, London.Kro¨ ner, A., Jaeckel, P. & Hegner, E., 2001. Single zircon ages<strong>and</strong> whole-rock Nd isotopic systematics <strong>of</strong> Early Palaeozoicgranitoid gneissess from the Czech <strong>and</strong> Polish Sudetes.(Jizerske´ Hory, Krkonosˇe mountains <strong>and</strong> Orlice-Sneˇzˇnı´ kcomplex). International Journal <strong>of</strong> Earth Sciences, 90, 304–324.Kryza, R., Pin, C. & Vielzeuf, D., 1996. High-pressure granulitesfrom the Sudetes (south-west Pol<strong>and</strong>): evidence <strong>of</strong> crustalsubduction <strong>and</strong> collisional thickening in the Variscan Belt.Journal <strong>of</strong> Metamorphic Geology, 14, 531–546.Lange, U., Bro¨ cker, M., Armstrong, R., Trapp, E. & Mezger,K., 2005. Sm–Nd <strong>and</strong> U–Pb dating <strong>of</strong> high-pressure granulitesfrom the Zlote <strong>and</strong> Rychleby Mts (Bohemian Massif, Pol<strong>and</strong><strong>and</strong> Czech Republic). Journal <strong>of</strong> Metamorphic Geology, 23,133–145.Lexa, O., Sˇtı´ pska´ , P., Schulmann, K., Baratoux, L. & Kro¨ ner,A., 2005. Contrasting textural record <strong>of</strong> two distinct metamorphicevents <strong>of</strong> similar P–T conditions <strong>and</strong> different durations.Journal <strong>of</strong> Metamorphic Geology, 23, 649–666.Macintyre, R. M., Bowes, D.R., Hamidullah, S. & Onscott,T.C., 1992. K–Ar <strong>and</strong> Ar–Ar study <strong>of</strong> amphibolites frommeta-ophiolite complexes, eastern Bohemian Massif. In: Proceedings<strong>of</strong> 1st International Conference on the BohemianMassif, Czech Geological Survey, Prague, pp. 195–199.Martinez, F., Goodliffe, A. M. & Taylor, B., 2001. Metamorphiccore complex formation by density inversion <strong>and</strong> lower crustextrusion. Nature, 411, 930–934.Matte, P., Maluski, H., Rajlich, P. & Franke, W., 1990. Terraneboundaries in the Bohemian Massif: result <strong>of</strong> large-scaleVariscan shearing. Tectonophysics, 177, 151–170.Mazur, S., Aleks<strong>and</strong>rowski, P. & Szczepanski, J., 2005. Thepresumed Tepla´ –Barr<strong>and</strong>ian ⁄ Moldanubian terrane boundaryin the Orlica Mountains (Sudetes, Bohemian Massif): <strong>structural</strong><strong>and</strong> petrological characteristics. Lithos, 82, 85–112.Medaris, G., Jelínek, E. & Mı´ sarˇ, Z., 1995. Czech eclogites:terrane settings <strong>and</strong> implications for Variscan tectonic evolution<strong>of</strong> the Bohemian Massif. European Journal <strong>of</strong> Mineralogy,7, 7–28.Medaris, L. G., Fournelle, J. H., Ghent, E. D., Jelínek, E. &Mı´ sarˇ, Z., 1998. Prograde eclogite in the Gfo¨ hl Nappe, CzechRepublic: new evidence on Variscan high-pressure metamorphism.Journal <strong>of</strong> Metamorphic Geology, 16, 563–576.Medaris, L. G., Beard, B. L. & Jelínek, E., 2006. Mantle-derived,UHP garnet pyroxenite <strong>and</strong> eclogite in the MoldanubianGfo¨ hl nappe, Bohemian Massif: a geochemical review, new P–T determinations, <strong>and</strong> tectonic interpretation. InternationalGeology Review, 48, 765–777.Milnes, A. G. & Koyi, H. A., 2000. Ductile rebound <strong>of</strong> anorogenic root: case study <strong>and</strong> <strong>numerical</strong> model <strong>of</strong> gravitytectonics in the Western Gneiss Complex, Caledonides,southern Norway. Terra Nova, 12, 1–7.Murtezi, M., 2006. The acid metavolcanic rocks <strong>of</strong> the Orlica–S´ niez_ nik Dome (Sudetes): their origin <strong>and</strong> tectono-metamorphicevolution. Geologica Sudetica, 38, 1–38.OÕBrien, P. J. & Carswell, D. A., 1993. Tectonometamorphicevolution <strong>of</strong> the Bohemian Massif: evidence from highpressure metamorphic rocks. Geologische Rundschau, 82,531–555.OÕBrien, P. J. & Ro¨ tzler, J., 2003. High-pressure granulites:formation, recovery <strong>of</strong> peak conditions <strong>and</strong> implications fortectonics. Journal <strong>of</strong> Metamorphic Geology, 21, 3–20.Parry, M., Sˇtı´ pska´ , P., Schulmann, K., Hrouda, F., Ježek, J. &Kro¨ ner, A., 1997. Tonalite sill emplacement at an obliqueplate boundary: northeastern margin <strong>of</strong> the Bohemian Massif.Tectonophysics, 280, 61–81.Petrakakis, K., 1997. Evolution <strong>of</strong> Moldanubian rocks in Austria:review <strong>and</strong> synthesis. Journal <strong>of</strong> Metamorphic Geology,15, 203–222.Pitra, P. & Guiraud, M., 1996. Probable anticlockwise P–Tevolution in extending crust: Hlinsko region, BohemianMassif. Journal <strong>of</strong> Metamorphic Geology, 14, 49–60.Pitra, P., Burg, J.-P., Schulmann, K. & Ledru, P., 1994. Lateorogenic extension in the Bohemian Massif: petro<strong>structural</strong>evidence in the Hlinsko region. Geodinamica Acta, 7, 15–30.Platt, J. P., 1986. Dynamics <strong>of</strong> orogenic wedges <strong>and</strong> the uplift <strong>of</strong>high-pressure metamorphic rocks. Geological Society <strong>of</strong>America Bulletin, 97, 1037–1053.Platt, J. P., 1993. Exhumation <strong>of</strong> high-pressure rocks: a review <strong>of</strong>concepts <strong>and</strong> processes. Terra Nova, 5, 119–133.Racek, M., Sˇtı´ pska´ , P., Pitra, P., Schulmann, K. & Lexa, O.,2006. Metamorphic record <strong>of</strong> burial <strong>and</strong> exhumation <strong>of</strong> orogeniclower <strong>and</strong> middle crust: a new tectonothermal model forthe Drosendorf window (Bohemian Massif, Austria). Mineralogy<strong>and</strong> Petrology, 86, 221–251.Rey, P., V<strong>and</strong>erhaeghe, O. & Teyssier, C., 2001. Gravitationalcollapse <strong>of</strong> the continental crust: definition, regimes <strong>and</strong>modes. Tectonophysics, 342, 435–449.Ó 2007 Blackwell Publishing Ltd156
EXHUMATION IN LARGE HOT OROGEN 297Ring, U. & Br<strong>and</strong>on, M. T., 1999. Ductile deformation <strong>and</strong> massloss in the Franciscan Subduction Complex: implications forexhumation processes in accretionary wedges. In: ExhumationProcesses: Normal Faulting, Ductile Flow <strong>and</strong> Erosion, SpecialPublication 154 (ed. Ring, U., Br<strong>and</strong>on, M.T., Lister, G.S. &Willet, S.D.), pp. 55–86. Geological Society, London.Romanova´ ,M.&Sˇtı´ pska´ , P., 2001. Structural <strong>and</strong> metamorphicevolution <strong>of</strong> the Stronie formation near Javorník. MineralogicalSociety <strong>of</strong> Pol<strong>and</strong>, Special Papers, 19, 147–149.Schneider, D. A., Zahniser, S. J., Clascock, J. M., Gordon, S. M.& Manecki, M., 2006. Thermochronology <strong>of</strong> the West Sudetes(Bohemian Massif): rapid <strong>and</strong> repeated eduction in the easternVariscides, Pol<strong>and</strong> <strong>and</strong> Czech Republic. American Journal <strong>of</strong>Science, 306, 846–873.Schulmann, K., 1990. Fabric <strong>and</strong> kinematic study <strong>of</strong> the Bitesorthogneiss (southwestern Moravia): result <strong>of</strong> large-scalenortheastward shearing parallel to the Moldanubian⁄ Moravian boundary. Tectonophysics, 177, 229–244.Schulmann, K. & Gayer, R., 2000. A model for a continentalaccretionary wedge developed by oblique collision: The NEBohemian Massif. Journal <strong>of</strong> the Geological Society, 157, 401–416.Schulmann, K., Ledru, P., Autran, A. et al., 1991. Evolution <strong>of</strong>nappes in the eastern margin <strong>of</strong> the Bohemian Massif: akinematic interpretation. Geologische Rundschau, 80, 73–92.Schulmann, K., Melka, R., Lobkowicz, M. Z., Ledru, P., Lardeaux,J.-M. & Autran, A., 1994. Contrasting styles <strong>of</strong>deformation during progressive nappe stacking at the southeasternmargin <strong>of</strong> the Bohemian Massif (Thaya Dome).Journal <strong>of</strong> Structural Geology, 16, 355–370.Schulmann, K., Schaltegger, U., Ježek, J., Thompson, A.B. &Edel, J.-B., 2002. Rapid burial <strong>and</strong> exhumation during orogeny:thickening <strong>and</strong> synconvergent exhumation <strong>of</strong> thermallyweakened <strong>and</strong> thinned crust (Variscan orogen in WesternEurope). American Journal <strong>of</strong> Science, 302, p 856–879.Schulmann, K., Thompson, A. B., Lexa, O. & Ježek, J., 2003.Strain distribution <strong>and</strong> fabric development modeled in active<strong>and</strong> ancient transpressive zones. Journal <strong>of</strong> GeophysicalResearch–Solid Earth, 108(B1), 2023, doi: 10.1029/200/JB000632./.Schulmann, K., Kroner, A., Hegner, E. et al., 2005. Chronologicalconstraints on the pre-orogenic history, burial <strong>and</strong>exhumation <strong>of</strong> deep-seated rocks along the eastern margin <strong>of</strong>the Variscan orogen, Bohemian Massif, Czech Republic.American Journal <strong>of</strong> Science, 305, 407–448.Steltenpohl, M. G., Cymerman, Z., Krogh, E. J. & Kunk, M. J.,1993. Exhumation <strong>of</strong> eclogitized continental basement duringVariscan lithospheric delamination <strong>and</strong> gravitational collapse,Sudety Mountains, Pol<strong>and</strong>. Geology, 21, 1111–1114.Sˇtı´ pska´ , P. & Powell, R., 2005a. Constraining the P–T path <strong>of</strong> aMORB-type eclogite using pseudosections, garnet zoning <strong>and</strong>garnet–clinopyroxene thermometry: an example from theBohemian Massif. Journal <strong>of</strong> Metamorphic Geology, 23, 725–743.Sˇtı´ pska´ , P. & Powell, R., 2005b. Does ternary feldspar constrainthe metamorphic conditions <strong>of</strong> high-grade meta-igneousrocks? Evidence from orthopyroxene granulites, BohemianMassif Journal <strong>of</strong> Metamorphic Geology, 23, 627–647.Sˇtı´ pská, P. & Schulmann, K., 1995. Inverted metamorphiczonation in a basement-derived nappe sequence, easternmargin <strong>of</strong> the Bohemian Massif. Geological Journal, 30, 385–413.Sˇtı´ pská, P., Schulmann, K. & Ho¨ ck, V., 2000. Complex metamorphiczonation <strong>of</strong> the Thaya dome: result <strong>of</strong> buckling <strong>and</strong>gravitational collapse <strong>of</strong> an imbricated nappe sequence. In:Forced Folds <strong>and</strong> Fractures, Special Publication, 169 (edsCosgrove, J. W. & Ameen, M. S.), pp. 197–211. GeologicalSociety, London.Sˇtı´ pská, P., Schulmann, K., Thompson, A. B., Ježek, J. & Kro¨ ner,A., 2001. Thermomechanical role <strong>of</strong> a Cambro–Ordovicianpaleorift during the Variscan collision: the NE margin <strong>of</strong> theBohemian Massif. Tectonophysics, 332, 239–253.Sˇtı´ pská, P., Schulmann, K. & Kro¨ ner, A., 2004. Vertical extrusion<strong>and</strong> middle crustal spreading <strong>of</strong> omphacite granulite: amodel <strong>of</strong> syn-convergent exhumation (Bohemian Massif,Czech Republic). Journal <strong>of</strong> Metamorphic Geology, 22, 179–198.Sˇtı´ pská, P., Pitra, P. & Powell, R., 2006. Separate or sharedmetamorphic histories <strong>of</strong> eclogites <strong>and</strong> surrounding rocks? Anexample from the Bohemian Massif Journal <strong>of</strong> MetamorphicGeology, 24, 219–240.Suess, F. E., 1912. Die moravischen Fenster und ihre Beziehungzum Grundgebirge des Hohen Gesenke. Denkschrichte desKoeniglischen Akademie der Wissenscahft, Mathematik.Naturwissenschaft, 12, 541–631.Suess, F. E., 1926. Intrusionstektonik und W<strong>and</strong>ertektonik imvariszichen Grundgebirge. Borntträger, Berlin.Tajčmanova´ , L., Konopa´ sek, J. & Schulmann, K., 2006. Thermalevolution <strong>of</strong> the orogenic lower crust during exhumationwithin a thickened Moldanubian root <strong>of</strong> the Variscan belt <strong>of</strong>Central Europe. Journal <strong>of</strong> Metamorphic Geology, 24, 119–134.Thompson, A. B., Schulmann, K., Jezˇek, J. & Tolar, V., 2001.Thermally s<strong>of</strong>tened continental extensional zones (arcs <strong>and</strong>rifts) as precursors to thickened orogenic belts. Tectonophysics,332, 115–141.Tollmann, A., 1982. Großraumiger variszischer Deckenbau imMoldanubikum und neue Gedanken zum Variszikum Europas.Geotektektonische Forschungen, 64, 1–91.Urban, M., 1992. Kinematics <strong>of</strong> the Variscan thrusting in theEastern Moldanubicum (Bohemian Massif, Czechoslovakia):evidence from the Namest granulite massif. Tectonophysics,201, 371–391.Van Breemen, O., Aftalion, M., Bowes, D. R. et al., 1982.Geochronological studies <strong>of</strong> the Bohemian massif, Czechoslovakia,<strong>and</strong> their significance in the evolution <strong>of</strong> CentralEurope. Transactions <strong>of</strong> the Royal Society <strong>of</strong> Edinburgh: EarthSciences, 73, 89–108.V<strong>and</strong>erhaeghe, O. & Teyssier, C., 2001. Partial melting <strong>and</strong> flow<strong>of</strong> orogens. Tectonophysics, 342, 451–472.Ziegler, P. A., 1986. Geodynamic model for the Palaeozoiccrustal consolidation <strong>of</strong> western <strong>and</strong> central Europe. Tectonophysics,126, 303–328.Received 3 April 2007; revision accepted 27 November 2007.Ó 2007 Blackwell Publishing Ltd157
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' ~'-----2~--~----TEXTURES OF NATUR
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TEXTURES OF NATURALLY DEFORMED META
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TEXTURES OF NATURALLY DEFORMED META
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TEXTURES OF NATURALLY DEFORMED META
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TEXTURES OF NATURALLY DEFORMED META
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TEXTURES OF NATURALLY DEFORMED META
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TEXTURES OF NATURALLY DEFORMED META
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B10210ZÁVADA ET AL.: EXTREME DUCTI
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B10210ZÁVADA ET AL.: EXTREME DUCTI
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B10210ZÁVADA ET AL.: EXTREME DUCTI
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B10210ZÁVADA ET AL.: EXTREME DUCTI
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ClickHereforFullArticleJOURNAL OF G
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B10406SCHULMANN ET AL.: RHEOLOGY OF
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B10406SCHULMANN ET AL.: RHEOLOGY OF
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B10406SCHULMANN ET AL.: RHEOLOGY OF
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B10406SCHULMANN ET AL.: RHEOLOGY OF
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J. metamorphic Geol., 2008, 26, 29-
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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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104 J. FRANĚK ET AL.in terms of th
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106 J. FRANĚK ET AL.Fig. 2. Struct
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108 J. FRANĚK ET AL.(a)perthite po
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110 J. FRANĚK ET AL.(a)(b)(c) (d)
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112 J. FRANĚK ET AL.Table 1. Repre
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114 J. FRANĚK ET AL.at these P-T c
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116 J. FRANĚK ET AL.(a)(b)Fig. 10.
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118 J. FRANĚK ET AL.(a)(b)Fig. 11.
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120 J. FRANĚK ET AL.Table 2. Quant
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122 J. FRANĚK ET AL.(a)(b)Fig. 15.
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124 J. FRANĚK ET AL.Fig. 16. Inter
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126 J. FRANĚK ET AL.development of
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128 J. FRANĚK ET AL.Behrmann, J.H.
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130 J. FRANĚK ET AL.Southern Bohem
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