Quantitative structural analyses and numerical modelling of ...

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3. Quantitative analyses of metamorphic microstructures 383.2 Accompanying publicationsLexa, O., Štípská, P., Schulmann, K., Baratoux, L., Kröner, A., 2005. Contrastingtextural record of two distinct metamorphic events of similar P-T conditions anddifferent durations. Journal of Metamorphic Geology 23 (8), 649–666. 231Baratoux, L., Schulmann, K., Ulrich, S., Lexa, O., 2005b. Contrasting microstructuresand deformation mechanisms in metagabbro mylonites contemporaneouslydeformed under different temperatures (c. 650°C and c. 750°C).; Deformationmechanisms, rheology and tectonics; from minerals to the lithosphere. Journalof Structural Geology 243 (4), 97–125. 249Závada, P., Schulmann, K., Konopásek, J., Ulrich, S., Lexa, O., 2007. Extremeductility of feldspar aggregates–melt-enhanced grain boundary sliding and creepfailure: rheological implications for felsic lower crust. Journal of Geophysical Research,B, Solid Earth and Planets 112, B10210, doi:10.1029/2006JB004820.279Schulmann, K., Martelat, J.-E., Ulrich, S., Lexa, O., Štípská, P., Becker, J. K., Oct.2008b. Evolution of microstructure and melt topology in partially molten graniticmylonite: Implications for rheology of felsic middle crust. Journal of GeophysicalResearch, B, Solid Earth and Planets 113, B10406, doi:10.1029/2007JB005508.295Hasalová, P., Schulmann, K., Lexa, O., Štípská, P., Hrouda, F., Ulrich, S., Haloda,J., Týcová, P., 2008a. Origin of migmatites by deformation-enhanced melt infiltrationof orthogneiss: a new model based on quantitative microstructural analysis.Journal of Metamorphic Geology 26, 29–53. 315Franěk, J., Schulmann, K., Lexa, O., Ulrich, S., Štípská, P., Haloda, J., Týcová, P.,2011b. Origin of felsic granulite microstructure by heterogeneous decomposition ofalkali feldspar and extreme weakening of orogenic lower crust during the Variscanorogeny. Journal of Metamorphic Geology 29 (1), 103–130. 3413.3 Related publicationsBarraud, J., 2006. The use of watershed segmentation and GIS software for texturalanalysis of thin sections. Journal of Volcanology and Geothermal Research 154 (1-2), 17–33.
3. Quantitative analyses of metamorphic microstructures 39Machek, M., Špaček, P., Ulrich, S., Heidelbach, F., 2007. Origin and orientationof microporosity in eclogites of different microstructure studied by ultrasound andmicrofabric analysis. Engineering Geology 89 (3-4), 266–277.Jeřábek, P., Stunitz, H., Heilbronner, R., Lexa, O., Schulmann, K., 2007. Microstructural- deformation record of an orogen-parallel extension in the Veporunit, West Carpathians. Journal of Structural Geology 29 (11), 1722–1743.Závada, P., Schulmann, K., Lexa, O., Hrouda, F., Haloda, J., Týcová, P., 2009. Themechanism of flow and fabric development in mechanically anisotropic trachytelava. Journal of Structural Geology 31 (11), 1295–1307.Skrzypek, E., Schulmann, K., Štípská, P., Chopin, F., Lehmann, J., Lexa, O.,Haloda, J., 2011a. Tectono-metamorphic history recorded in garnet porphyroblasts:insights from thermodynamic modelling and electron backscatter diffractionanalysis of inclusion trails. Journal of Metamorphic Geology 29 (4), 473–496.Chopin, F., Schulmann, K., Štípská, P., Martelat, J., Pitra, P., Lexa, O., Petri,B., 2011b. Microstructural and petrological evolution of a high pressure graniticorthogneiss during continental subduction (Orlica-Śnieżnik dome, NE BohemianMassif). Journal of Metamorphic Geology, submitted.Oliot, E., Lexa, O., Schulmann, K., Goncalves, P., Marquer, D., 2011. Mid-crustalstrain localization in granitic rocks: constraints from quantitative textural andcrystallographic preferred orientations analyses. Tectonophysics, submitted.Martelat, J.-E., Malamoud, K., Cordier, B., Randrianasolo, B., Schulmann, K.,Lardeaux, J.-M., 2011. Garnet crystal plasticity in the continental crust, new examplefrom south Madagascar. Journal of Metamorphic Geology, submitted.
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 58 and 59: Bibliography 46Skrzypek, E., Štíp
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DTD 5ARTICLE IN PRESSJournal of Str
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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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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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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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