Quantitative structural analyses and numerical modelling of ...

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ForewordThis habilitation thesis consists of three main parts, which aim to underline the principaldirections and features of my scientific career and gives the overview of new scientificdirections, which I would like to follow as an associate professor of the Charles University.My research career is based on collaborative work of a larger research team, whichworked at the Institute of Petrology and Structural Geology from 1995 to 2011 and myresearch interest and focus was necessarily influenced by the overall aim of that group.This was particularly expressed in mathematical modelling of continental deformationin the micro-, meso - and macro-scale and the development of the necessary softwaretools for specific geologically oriented quantitative studies, which were published underthe Institute of Petrology and Structural Geology mostly in collaboration with K. Schulmann,J. Konopásek, P. Jeřábek, P. Štípská, S. Ulrich and others, who initiate manysubjects further discussed in this text. My skills in computer programs development,computer-based processing and statistical evaluation of structural data, implementationof database and geographic information systems and ability to model processes numericallyallowed me substantially contribute to several manuscripts of different authors thatare cited in this habilitation thesis. As these techniques were progressively more andmore used by IPSG research team, it became the driving force for three major researchdirections of my career presented here. These are following themes: 1) quantitativeanalysis of deformation structures and numerical modelling of deformation,2) mechanisms of lower crustal flow and its thermal and mechanical implicationsand 3) quantitative analysis of metamorphic microstructures, their visualizationand statistical processing. At this point I would like to stress that I highlyappreciated multidisciplinary approach of collective scientific collaboration, which ruledin the last ten years of my professional career in the Institute of Petrology and StructuralGeology and that helped me to identify the essentials of my personal approach, as wellas the professional qualities of my colleagues. It is my aim further transfer this spirit ofactive cooperation and stimulating discussions to students and cultivate this approachat Charles University in the future.1
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 15 and 16: Foreword 32008, 2007) and subsequen
Page 17 and 18: Chapter 1Quantitative analysis ofde
Page 19 and 20: 1. Quantitative analysis of deforma
Page 29: 1. Quantitative analysis of deforma
Page 32 and 33: 2. Mechanisms of lower crustal flow
Page 42 and 43: 3. Quantitative analyses of metamor
Page 53 and 54: BibliographyAerden, D., 1998. Tecto
Page 55 and 56: Bibliography 43Jeřábek, P., Farya
Page 57 and 58: Bibliography 45Petrology 86 (3-4),
Page 59: Accompanying publications47
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1374J. KonopaÂsek et al. / Journal
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ETG 6 - 2 SCHULMANN ET AL.: STRAIN
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TECTONICS, VOL. 22, NO. 6, 1066, do
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LEXA ET AL.: COLLISION IN WEST CARP
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Journal of Structural Geology 26 (2
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O. Lexa et al. / Journal of Structu
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DTD 5ARTICLE IN PRESS2L. Baratoux e
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DTD 5ARTICLE IN PRESS10L. Baratoux
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DTD 5 ARTICLE IN PRESS14L. Baratoux
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274 K. SCHULMANN ET AL.orogenic roo
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276 K. SCHULMANN ET AL.Moldanubian-
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278 K. SCHULMANN ET AL.Fig. 4. P-T
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280 K. SCHULMANN ET AL.gneisses, mi
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282 K. SCHULMANN ET AL.characterize
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284 K. SCHULMANN ET AL.(a)(b)OrMeOm
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286 K. SCHULMANN ET AL.Fig. 8. Fiel
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288 K. SCHULMANN ET AL.(d)(c)PrRe(b
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290 K. SCHULMANN ET AL.top-to-the-N
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292 K. SCHULMANN ET AL.example in t
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294 K. SCHULMANN ET AL.at 330-325 M
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296 K. SCHULMANN ET AL.thermal and
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Author's personal copyC. R. Geoscie
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Author's personal copy268K. Schulma
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80 O. LEXA ET AL.rocks (greenstone
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82 O. LEXA ET AL.(a)(a´)(b)(b´)(a
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84 O. LEXA ET AL.mechanism lead to
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86 O. LEXA ET AL.(a)(b)(c)and high-
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88 O. LEXA ET AL.Fig. 7. Results of
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90 O. LEXA ET AL.Fig. 8. Results of
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92 O. LEXA ET AL.Fig. 10. P-T evolu
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94 O. LEXA ET AL.(a)(b)(c)(d)Fig. 1
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96 O. LEXA ET AL.subsolidus conditi
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98 O. LEXA ET AL.of momentum (Eqn A
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100 O. LEXA ET AL.Hasalova´, P., S
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102 O. LEXA ET AL.(Bohemian Massif)
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54 J. FRANĚK ET AL.represented mos
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56 J. FRANĚK ET AL.Fig. 2. Summary
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58 J. FRANĚK ET AL.to c. 346 Ma (J
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60 J. FRANĚK ET AL.(a)(b)(c)(d)Fig
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62 J. FRANĚK ET AL.Fig. 7. Equal a
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64 J. FRANĚK ET AL.Fig. 9. The 9HR
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66 J. FRANĚK ET AL.At the top, the
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68 J. FRANĚK ET AL.Fig. 12. Interp
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70 J. FRANĚK ET AL.and underlying
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72 J. FRANĚK ET AL.Bohemian Pluton
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74 J. FRANĚK ET AL.weak lower and
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76 J. FRANĚK ET AL.Janousˇek, V.,
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78 J. FRANĚK ET AL.Weber, K., 1984
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650 O. LEXA ET AL.followed by moder
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652 O. LEXA ET AL.(a)(b)Fig. 3. Geo
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654 O. LEXA ET AL.(a)(b)(c)(d)Fig.
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656 O. LEXA ET AL.Table 2. Summariz
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658 O. LEXA ET AL.Table 5. Represen
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660 O. LEXA ET AL.Fig. 7. Chemical
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662 O. LEXA ET AL.Fig. 9. (a) Plot
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664 O. LEXA ET AL.onset of dynamic
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666 O. LEXA ET AL.clase thermometry
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98 L. BARATOUX ETAL.bearing rocks a
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100 L. BARATOUX ETAL.regime but und
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102 L. BARATOUX ETAL.is observed wi
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104 L. BARATOUX ETAL.only 10-20% of
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106 L. BARATOUX ET AL.Fig. 7. Drawi
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108 L. BARATOUX ET AL.Fig. 9. BSE i
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110 L. BARATOUX ETAL.r~t'-,IMdMdddd
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112 L. BARATOUX ET AL.Quantitative
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114 L. BARATOUX ETAL.o ._,
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116 L. BARATOUX ETAL.Plagioclase -
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118 L. BARATOUX ETAL.Plagioclase -
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120 L. BARATOUX ET AL.are contempor
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122 L. BARATOUX ET AL.recrystallize
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124 L. BARATOUX ETAL.KNIPE, R. J. 1
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ClickHereforFullArticleJOURNAL OF G
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B10210ZÁVADA ET AL.: EXTREME DUCTI
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B10406SCHULMANN ET AL.: RHEOLOGY OF
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30 P. HASALOVÁ ET AL.These authors
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32 P. HASALOVÁ ET AL.The onset of
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34 P. HASALOVÁ ET AL.Table 1. Repr
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36 P. HASALOVÁ ET AL.Evidence of m
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38 P. HASALOVÁ ET AL.PlQtz70% 30%B
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40 P. HASALOVÁ ET AL.(a)(b)(c)Fig.
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42 P. HASALOVÁ ET AL.Fig. 9. Grain
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44 P. HASALOVÁ ET AL.(a)(b)Fig. 11
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46 P. HASALOVÁ ET AL.steep D 1 fab
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48 P. HASALOVÁ ET AL.refractory. I
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50 P. HASALOVÁ ET AL.creep and gra
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52 P. HASALOVÁ ET AL.Lafeber, D.,
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J. metamorphic Geol., 2011, 29, 103
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PRECURSOR AND RHEOLOGY OF VARISCAN
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