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1. Quantitative analysis of deformation structures and their numerical modelling 161.2 Accompanying publicationsKonopásek, J., Schulmann, K., Lexa, O., 2001. Structural evolution of the centralpart of the Krušné Hory (Erzgebirge) Mountains in the Czech Republic; evidencefor changing stress regime during Variscan compression. Journal of Structural Geology23 (9), 1373–1392. 49Schulmann, K., Thompson, A. B., Lexa, O., Ježek, J., 2003. Strain distributionand fabric development modeled in active and ancient transpressive zones. Journalof Geophysical Research, B, Solid Earth and Planets 108(B1), 2023, doi:10.1029/2001JB000632. 69Lexa, O., Schulmann, K., Ježek, J., 2003. Cretaceous collision and indentationin the Western Carpathians: View based on structural analysis and numericalmodeling. Tectonics 22 (6), 1066, doi:10.1029/2002TC001472. 85Lexa, O., Cosgrove, J., Schulmann, K., 2004. Apparent shear-band geometry resultingfrom oblique fold sections. Journal of Structural Geology 26 (1), 155–161.101Baratoux, L., Lexa, O., Cosgrove, J. W., Schulmann, K., 2005a. The quantitativelink between fold geometry, mineral fabric and mechanical anisotropy; as exemplifiedby the deformation of amphibolites across a regional metamorphic gradient.Journal of Structural Geology 27 (4), 707–730. 1091.3 Related publicationsKonopásek, J., Schulmann, K., Lexa, O., 2003. Reply to comments by A. Krohe andA.P. Willner on ”Structural evolution of the central part of the Kru né Hory (Erzgebirge)Mountains in the Czech Republic—evidence for changing stress regime duringVariscan compression”. Journal of Structural Geology 25 (6), 1005–1007. Schulmann, K., Edel, J.-B., Hasalová, P., Cosgrove, J., Ježek, J., Lexa, O., 2009a.Influence of melt induced mechanical anisotropy on the magnetic fabrics and rheologyof deforming migmatites, Central Vosges, France. Journal of Structural Geology31 (10), 1223–1237.Lehmann, J., Schulmann, K., Edel, J.-B., Hrouda, F., Lexa, O., Štípská, P., Haloda,J., 2011. AMS and structural record of granitoid sills emplacement during growthof continental gneiss dome: implications for exhumation of deep crust. Journal ofStructural Geology, submitted.
1. Quantitative analysis of deformation structures and their numerical modelling 17 Kratinová, Z., Ježek, J., Schulmann, K., Hrouda, F., Shail, R. K., Lexa, O., 2010.Noncoaxial K-feldspar and AMS subfabrics in the Land’s End granite, Cornwall:Evidence of magmatic fabric decoupling during late deformation and matrix crystallization.Journal of Geophysical Research, B, Solid Earth and Planets 115,B09104, doi:10.1029/2009JB006714.
Page 3: “It strikes me that all our knowl
Page 8 and 9: Contentsviii4.7 Schulmann, Konopás
Page 11: Dedicated to my wife Markéta, daug
Page 14 and 15: Foreword 2First topic “Quantitati
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Page 31 and 32: Chapter 2Mechanisms of lower crusta
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Page 54 and 55: Bibliography 42Culshaw, N., Beaumon
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Page 58 and 59: Bibliography 46Skrzypek, E., Štíp
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JOURNAL OF GEOPHYSICAL RESEARCH, VO
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SCHULMANN ET AL.: STRAIN DISTRIBUTI
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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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EXHUMATION IN LARGE HOT OROGEN 285a
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EXHUMATION IN LARGE HOT OROGEN 287w
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EXHUMATION IN LARGE HOT OROGEN 289T
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EXHUMATION IN LARGE HOT OROGEN 291O
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EXHUMATION IN LARGE HOT OROGEN 293r
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EXHUMATION IN LARGE HOT OROGEN 295B
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EXHUMATION IN LARGE HOT OROGEN 297R
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Author's personal copyK. Schulmann
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HEAT SOURCES AND EXHUMATION MECHANI
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EXTRUSIONOFLOWERCRUSTINVARISCANOROG
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J. metamorphic Geol., 2005, 23, 649
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CONTRASTING TEXTURAL RECORD OF TWO
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Contrasting microstructures and def
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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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' ~'-----2~--~----TEXTURES OF NATUR
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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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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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120 J. FRANĚK ET AL.Table 2. Quant
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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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