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ETG 6 - 2 SCHULMANN ET AL.: STRAIN DISTRIBUTIONthus allowing extrusion only in the vertical direction.Fossen and Tikoff [1998] suggested boundary conditionswhere zones of transpressive deformation are able to growthor shrink vertically as well as horizontally along strike.[5] Fossen and Tikoff [1993] defined two types of transpressionon the basis of the orientation of the instantaneousstretching axes: (1) pure-shear-dominated transpression inwhich v 1 and v 3 (eigenvectors of instantaneous straincorresponding to maximum and minimum elongation)define a vertical plane and the v 1 (lineation) is vertical,and (2) wrench-dominated transpression in which v 1 and v 3are horizontal, while the v 2 (intermediate eigenvector) isvertical. Pure-shear-dominated transpression operates whenthe angle between relative plate convergence direction andplate boundary is greater than 20° [Pinet and Cobbold,1992], and the main axis of finite strain is always vertical. Inwrench-dominated transpression acting at an angle of convergence(a) of
SCHULMANN ET AL.: STRAIN DISTRIBUTION ETG 6 - 3Figure 1. Block diagrams and principal strain axes orientations for transpressive systems with externalparameters: (a) plate velocity (v = 1 to 10 cm yr 1 ) and initial width (d = 50 to 300 km), which give theratio R vd from 2 to 0.03, respectively, and rigid floor depth (RFD = 70, 40 km). As internal parameters,the instantaneous orientation of foliation plane (XY ) and lineation (X ) are related to angle of convergence(a) of(c)a =60° and (d) a
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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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Page 58 and 59: Bibliography 46Skrzypek, E., Štíp
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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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J. metamorphic Geol., 2011, 29, 79-
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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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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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