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DTD 5 ARTICLE IN PRESS14L. Baratoux et al. / Journal of Structural Geology xx (xxxx) 1–24Fig. 8. Typical microstructures from the four metamorphic zones, redrawn and digitized in the ArcView GIS environment. The rose diagrams represent grain long axis distribution. Full symbols correspond tofold limbs, open symbols to fold hinges. These symbols have the same significance in Figs. 9 and 11. The minerals can be identified as follows: plagioclase—white; amphibole—medium grey; spheneCilmenomagnetite—black; quartz—vertically hatched; calcite—dotted; clinopyroxene—light grey.122
Table 1Statistical values of the quantitative textural analysisZone Grt St SilSil (plutonaureole)Sample 162 163 84 84 10 10 149 4Limb Hinge Limb Hinge Limb Hinge Limb HingeGBPO Pl–pl 1.06 1.10 1.21 1.21 1.25 1.12 1.10 1.22Eigenvalue rZ Amp–amp 2.12 1.47 2.39 1.43 1.76 1.70 1.23 1.22e1/e2Amp–pl 1.45 1.17 1.95 1.26 1.48 1.52 1.33 1.08Eigenvector Pl–pl K25 K74 22 88 K9 K65 28 83orientation (8) a Amp–amp K11 K22 K3 K76 K11 K77 74 K83Amp–pl K16 K2 K4 89 K14 K78 91 K73SPO Pl 1.21 1.06 1.57 1.25 1.42 1.44 1.23 1.16Eigenvalue r Amp 2.39 1.57 3.06 1.44 2.16 1.88 1.44 1.31Eigenvector Pl K16 K38 1 K90 K9 K81 89 K90orientation (8) a Amp K11 K3 K6 K88 K15 K79 79 K86Aspect ratio Pl 1.46 1.48 1.64 1.53 1.59 1.76 1.49 1.41(median)Amp 2.05 1.81 2.17 1.89 2.03 2.36 1.57 1.60Grain size—FerretdiameterMedian (mm) Pl 17 22 17 15 39 28 65 35Amp 31 33 21 20 64 46 80 43Q1 (mm) Pl 11 14 10 10 27 20 36 21Amp 16 18 13 13 38 29 45 29Q 3 (mm) Pl 25 34 25 21 52 39 114 53Amp 75 59 35 32 104 79 130 65Q3KQ1 (mm) Pl 14 20 15 12 25 19 79 33Amp 59 41 22 19 66 49 85 37a Positive values are oriented anticlockwise with respect to the horizontal.L. Baratoux et al. / Journal of Structural Geology xx (xxxx) 1–24 15DTD 5 ARTICLE IN PRESS123
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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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HEAT SOURCES AND EXHUMATION MECHANI
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CONTRASTING TEXTURAL RECORD OF TWO
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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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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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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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112 J. FRANĚK ET AL.Table 1. Repre
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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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