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1374J. KonopaÂsek et al. / Journal of Structural Geology 23 2001) 1373±1392Fig. 1. a) Location of the KrusÏneÂ hory Mountains in the European Variscides black square in the northern part of the Bohemian Massif). b) Simpli®edgeological map of the central part of the KrusÏneÂ hory Mountains with the studied area outlined by a black line.event responsible for the building of the ®nal geologicalpattern.In this paper we document that the structural fabric associatedwith emplacement of a crustal nappe is later affectedby an important N±S compression, which is responsible forregional-scale refolding of a previously developed ¯at lyingfoliation. We discuss the succession of deformational eventsin conjunction with the thermal evolution and changingstress regimes through time. We also correlate small-scalestructures and observed ®nite strain ellipsoids with stressesoperating during the crustal-scale folding associated withexhumation of the middle crust.2. Geological settingThe Bohemian Massif represents the easternmost crystallinecomplex of the European Variscides. Its western part iscomposed of the Saxothuringian domain, which has beenalready recognised by Kossmat 1927) as a unit with adistinct lithological and stratigraphic evolution with respectto the more easterly lying unitsÐthe TeplaÂ±Barrandian andthe Moldanubian domains.The area studied is situated in the central part of theKrusÏneÂ hory Mountains Erzgebirge), which representthe easternmost termination of the Saxothuringian domain.50
J. KonopaÂsek et al. / Journal of Structural Geology 23 2001) 1373±1392 1375Fig. 2. Synoptic geological map of the studied area simpli®ed after Sattran 1967) and Hoth et al. 1994)). The inset represents lithotectonic column. Solid black lines show the position of cross-sectionspresented in Fig. 3.51
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“It strikes me that all our knowl
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Contentsviii4.7 Schulmann, Konopás
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Page 58 and 59: Bibliography 46Skrzypek, E., Štíp
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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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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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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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