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94 O. LEXA ET AL.(a)(b)(c)(d)Fig. 11. Model proposed for the tectonic evolution of the orogenic root domain in the Bohemian Massif. (a) Model of continentalunderthrusting with development of the Barrandian forearc region, CBPC magmatic arc and backarc region represents the futureMoldanubian domain. The position of the Palaeotethys suture is indicated as the future Maria´nské La´zneˇ Complex. (b) Relaminationmodel with part of the allochthonous Saxothuringian crust injected between the Moho and the continental lithosphere. The other partis subducted thereby producing metasomatism of the overlying mantle. (c) Crustal thickening of the former backarc domain(Schulmann et al., 2005, 2009). (d) Vertical extrusion and gravity redistribution of relaminated Saxothuringian crust at the end ofVariscan orogeny.Ó 2010 Blackwell Publishing Ltd196
HEAT SOURCES AND EXHUMATION MECHANISMS 95(a) (b)Fig. 12. (a) Pseudosection for granulite sample H296-S1 (Blanský les Massif) to show the P–T path from the peak assemblage of g–ky–pl–ksp–q–liq–ru at 16 kbar and 860 °C bydecompression to 8 kbar and 820 °C (modified from Franeˇk et al., 2011b). Molar percentage of melt is very low and allows the preservation of the peak assemblage ondecompression and cooling. (b) Pseudosection for sample H296-S1 with 7 mol.% of melt added allows the stability of the mu–bi–pl–ksp–q assemblage at subsolidus conditions.Such a reconstructed granite whole-rock and mineral composition predicts 8 mol.% of melt at peak P–T conditions and 12 mol.% of melt at 8 kbar and 860 °C. Some melt mustbe lost to preserve the peak g–ky–pl–ksp–q–liq–ru assemblage.Ó 2010 Blackwell Publishing Ltd197
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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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Journal of Structural Geology 23 20
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DTD 5ARTICLE IN PRESSJournal of Str
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DTD 5ARTICLE IN PRESSL. Baratoux et
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Table 1Statistical values of the qu
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Table 2Summary of parameters derive
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J. metamorphic Geol., 2008, 26, 273
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EXHUMATION IN LARGE HOT OROGEN 275m
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Probabi l irequencyProbabi l ireque
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EXHUMATION IN LARGE HOT OROGEN 279y
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EXHUMATION IN LARGE HOT OROGEN 281N
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EXHUMATION IN LARGE HOT OROGEN 283w
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TEXTURES OF NATURALLY DEFORMED META
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1.0--0.9__Mg~(Mg2++Fe2+)9 Core of p
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ClickHereforFullArticleJOURNAL OF G
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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 43(a)(b
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ORIGIN OF FELSIC MIGMATITES 45Fig.
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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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128 J. FRANĚK ET AL.Behrmann, J.H.
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130 J. FRANĚK ET AL.Southern Bohem
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