128 J. FRANĚK ET AL.Behrmann, J.H. & Mainprice, D., 1987. Deformation mechanismsin a high-temperature quartz-feldspar mylonite: evidencefor super-plastic flow in the lower crust. Tectonophysics,140, 297–305.Boullier, A.M. & Gueguen, Y., 1975. SP-mylonites; origin <strong>of</strong>some mylonites by superplastic flow. Contributions to Mineralogy<strong>and</strong> Petrology, 50, 93–104.Brown, W.L. & Parsons, I., 1989. Alkali feldspars: orderingrates, phase transformations <strong>and</strong> behaviour diagrams forigneous rocks. Mineralogical Magazine, 53, 25–42.Carswell, D.A. & OÕBrien, P.J., 1993. Thermobarometry <strong>and</strong>geotectonic significance <strong>of</strong> high-pressure granulites – examplesfrom the Moldanubian Zone <strong>of</strong> the Bohemian Massif inLower Austria. Journal <strong>of</strong> Petrology, 34, 427–459.Casey, M., Kunze, K. & Olgaard, D.L., 1998. Texture <strong>of</strong> Solnh<strong>of</strong>enlimestone deformed to high strains in torsion. Journal<strong>of</strong> Structural Geology, 20, 255–267.Cashman, K.V. & Ferry, J.M., 1988. Crystal size distribution(CSD) in rocks <strong>and</strong> the kinetics <strong>and</strong> dynamics <strong>of</strong> crystallization– III. Metamorphic crystallization. Contributions toMineralogy <strong>and</strong> Petrology, 99, 401–415.Coggon, R. & Holl<strong>and</strong>, T., 2002. Mixing properties <strong>of</strong> phengiticmicas <strong>and</strong> revised garnet-phengite thermobarometers. Journal<strong>of</strong> Metamorphic Geology, 20, 683–696.Cooke, R.A., 2000. High-pressure ⁄ temperature metamorphismin the St. Leonhard Granulite Massif, Austria: evidence fromintermediate pyroxene-bearing granulites. International Journal<strong>of</strong> Earth Sciences, 89, 647–651.DellÕAngelo, L.N., Tullis, J. & Yund, R.A., 1987. Transitionfrom dislocation creep to melt-enhanced diffusion creepin fine-grained granitic aggregates. Tectonophysics, 139, 325–332.DeVore, G.W., 1959. Role <strong>of</strong> minimum interfacial free energy indetermining the macroscopic features <strong>of</strong> mineral assemblages.I. The model. Journal <strong>of</strong> Geology, 67, 211–227.Diener, J.F.A., White, R.W. & Powell, R., 2008. Granulite faciesmetamorphism <strong>and</strong> subsolidus fluid-absent reworking,Strangways Range, Arunta Block, central Australia. Journal<strong>of</strong> Metamorphic Geology, 26, 603–622.Fiala, J., Mateˇjovska´, O.&Vanˇkova´, V., 1987. Moldanubiangranulites: source material <strong>and</strong> petrogenetic considerations.Neues Jahrbuch fur Mineralogie, Abh<strong>and</strong>lungen, 157, 133–165.Finger, F., Cooke, R., Janousˇek, V. et al., 2003. Petrogenesis <strong>of</strong>the south Bohemian granulites: the importance <strong>of</strong> crystal-meltrelationships. Journal <strong>of</strong> the Czech Geological Society, 48, 44–45.Flin, D., 1969. Grain contacts in crystalline rocks. Lithos, 2, 361–370.Franeˇk, J., Schulman, K. & Lexa, O., 2006. Kinematic <strong>and</strong>rheological model <strong>of</strong> exhumation <strong>of</strong> high pressure granulites inthe Variscan orogenic root: example <strong>of</strong> the Blansky´ les granulite,Bohemian Massif, Czech Republic. Mineralogy <strong>and</strong>Petrology, 86, 253–276.Franeˇk, J., Schulman, K., Lexa, O., Tomek, C. & Edel, J.B.,2011. Model <strong>of</strong> syn-convergent extrusion <strong>of</strong> orogenic lowercrust in the core <strong>of</strong> the Variscan belt: implications forexhumation <strong>of</strong> high-pressure rocks in large hot orogens.Journal <strong>of</strong> Metamorphic Geology, 29, 53–78.Franke, W., 2000. The mid-European segment <strong>of</strong> the Variscides:tectonostratigraphic units, terrane boundaries <strong>and</strong> plate tectonicevolution. Geological Society Special Publication, 179,35–56.Friedl, G., Cooke, R., Finger, F., McNaughton, N.J. & Fletcher,I., 2003. U-Pb SHRIMP dating <strong>and</strong> trace element investigationson multiple zoned zircons from a South-Bohemiangranulite. Journal <strong>of</strong> the Czech Geological Society, 48, 51.Fuchs, G., 1976. Zur Entwicklung der Bo¨ hmischen Masse.Jahrbuch des Geologischen Bundesanstalts, 119, 45–61.Garlick, S.R. & Gromet, L.P., 2004. Diffusion creep <strong>and</strong> partialmelting in high temperature mylonitic gneisses, Hope Valleyshear zone, New Engl<strong>and</strong> Appalachians, USA. Journal <strong>of</strong>Metamorphic Geology, 22, 45–62.Gayk, T. & Kleinschrodt, R., 2000. Hot contacts <strong>of</strong> garnetperidotites in middle ⁄ upper crustal levels: new constraints onthe nature <strong>of</strong> the late Variscan high-T ⁄ low-P event in theMoldanubian (Central Vosges ⁄ NE France). Journal <strong>of</strong> MetamorphicGeology, 18, 293–305.H<strong>and</strong>y, M., 1990. The solid state flow <strong>of</strong> polymineralic rocks.Journal <strong>of</strong> Geophysical Research, 95, 8647–8661.Hasalová, P., Sˇtı´pska´, P., Powell, R., Schulmann, K., Janousˇek,V. & Lexa, O., 2008a. Transforming mylonitic metagranite byopen-system interactions during melt flow. Journal <strong>of</strong> MetamorphicGeology, 26, 55–80.Hasalová, P., Schulmann, K., Lexa, O. et al., 2008b. Origin <strong>of</strong>migmatites by deformation-enhanced melt infiltration <strong>of</strong>orthogneiss: a new model based on quantitative micro<strong>structural</strong>analysis. Journal <strong>of</strong> Metamorphic Geology, 26, 29–53.Hay, R.S. & Evans, B., 1987. Chemically induced grain boundarymigration in calcite: temperature dependence, phenomenology,<strong>and</strong> possible applications to geologic systems.Contributions to Mineralogy <strong>and</strong> Petrology, 97, 127–141.Higgins, M.D., 1998. Origin <strong>of</strong> anorthosite by textural coarsening:quantitative measurements <strong>of</strong> a natural sequence <strong>of</strong>textural development. Journal <strong>of</strong> Petrology, 39, 1307–1323.Holl<strong>and</strong>, T. & Powell, R., 1998. An internally consistent thermodynamicdata set for phases <strong>of</strong> petrological interest. Journal<strong>of</strong> Metamorphic Geology, 16, 309–343.Holl<strong>and</strong>, T. & Powell, R., 2003. Activity–composition relationsfor phases in petrological calculations: an asymmetric multicomponentformulation. Contributions to Mineralogy <strong>and</strong>Petrology, 145, 492–501.Jakesˇ, P., 1997. Melting in high-P region – case <strong>of</strong> Bohemiangranulites. Acta Universitatis Carolinae, Geologica, 41, 113–125.Janousˇek, V. & Holub, F.V., 2007. The causal link between HP-HT metamorphism <strong>and</strong> ultrapotassic magmatism in collisionalorogens: case study from the Moldanubian Zone <strong>of</strong> theBohemian Massif. Proceedings <strong>of</strong> the Geologists Association,118, 75–86.Janousˇek, V., Finger, F., Roberts, M., Fry´da, J., Pin, C. &Dolejsˇ, D., 2004. Deciphering the petrogenesis <strong>of</strong> deeplyburied granites: whole-rock geochemical constraints onthe origin <strong>of</strong> largely undepleted felsic granulites from theMoldanubian Zone <strong>of</strong> the Bohemian Massif. Transactions <strong>of</strong>the Royal Society <strong>of</strong> Edinburgh – Earth Sciences, 95, 141–159.Janousˇek, V., Gerdes, A., Vrána, S. et al., 2006. Low-pressuregranulites <strong>of</strong> the Lisˇov Massif, Southern Bohemia: viseanmetamorphism <strong>of</strong> Late Devonian plutonic arc rocks. Journal<strong>of</strong> Petrology, 47, 705–744.Jiang, Z., Prior, D.J. & Wheeler, J., 2000. Albite crystallographicpreferred orientation <strong>and</strong> grain misorientation distribution ina low-grade mylonite: implications for granular flow. Journal<strong>of</strong> Structural Geology, 22, 1663–1674.Knipe, R.J., 1989. Deformation mechanisms – recognitionfrom natural tectonites. Journal <strong>of</strong> Structural Geology, 11,127–146.Kodym, O., 1972. Multiphase deformation in the Blanský lesgranulite massif (South Bohemia). Krystalinikum, 9, 91–105.Kosˇler, J., Kelley, S.P., Vance, D. & Svojtka, M., 1999. Independentdating <strong>of</strong> cooling <strong>and</strong> decompression <strong>of</strong> high graderocks in the southern Bohemian Massif with Ar-Ar, Sm-Nd<strong>and</strong> U-Pb techniques. Journal <strong>of</strong> Conference Abstracts, 4, 39.Kotkova´, J. & Harley, S.L., 1999. Formation <strong>and</strong> evolution <strong>of</strong>high-pressure leucogranulites: experimental constraints <strong>and</strong>unresolved issues. Physics <strong>and</strong> Chemistry <strong>of</strong> the Earth Part A –Solid Earth <strong>and</strong> Geodesy, 24, 299–304.Kretz, R., 1969. On the spatial distribution <strong>of</strong> crystals in rocks.Lithos, 2, 39–65.Kro¨ ner, A., OÕBrien, P.J., Nemchin, A.A. & Pidgeon, R.T.,2000. Zircon ages for high pressure granulites from SouthBohemia, Czech Republic, <strong>and</strong> their connection to Carboniferoushigh temperature processes. Contributions to Mineralogy<strong>and</strong> Petrology, 138, 127–142.Ó 2010 Blackwell Publishing Ltd366
PRECURSOR AND RHEOLOGY OF VARISCAN GRANULITES 129Kruse, R., Stunitz, H. & Kunze, K., 2001. Dynamic recrystallizationprocesses in plagioclase porphyroclasts. Journal <strong>of</strong>Structural Geology, 23, 1781–1802.Lexa, O., Sˇtı´pska´, P., Schulmann, K., Baratoux, L. & Kro¨ ner,A., 2005. Contrasting textural record <strong>of</strong> two distinct metamorphicevents <strong>of</strong> similar P–T conditions <strong>and</strong> different durations.Journal <strong>of</strong> Metamorphic Geology, 23, 649–666.Lexa, O., Schulmann, K., Janousˇek, V., Sˇtı´pska´, P., Guy, A. &Racek, M., 2011. Heat sources <strong>and</strong> trigger mechanisms <strong>of</strong>exhumation <strong>of</strong> HP granulites in Variscan orogenic root.Journal <strong>of</strong> Metamorphic Geology, 29, 79–102.Lister, G.S. & Dornsiepen, U.F., 1982. Fabric transition in theSaxony granulite terrain. Journal <strong>of</strong> Structural Geology, 4, 81–92.Lister, G.S. & Price, G.P., 1978. Fabric development in aquartz–feldspar mylonite. Tectonophysics, 49, 37–78.Marsh, B.D., 1988. Crystal size distributions (CSD) in rocks <strong>and</strong>the kinetics <strong>and</strong> dynamics <strong>of</strong> crystallization – I. Theory.Contributions to Mineralogy <strong>and</strong> Petrology, 99, 277–291.Martelat, J.E., Schulmann, K., Lardeaux, J.M., Nicollet, C. &Cardon, H., 1999. Granulite micr<strong>of</strong>abrics <strong>and</strong> deformationmechanisms in southern Madagascar. Journal <strong>of</strong> StructuralGeology, 21, 671–687.Matte, P., Maluski, H., Rajlich, P. & Franke, W., 1990. Terraneboundaries in the Bohemian Massif: result <strong>of</strong> the large–scaleVariscan shearing. Tectonophysics, 177, 151–170.Mehnert, K.R., 1968. Migmatites <strong>and</strong> the Origin <strong>of</strong> GraniticRocks. Elsevier, Amsterdam, 393 pp.Montardi, Y. & Mainprice, D., 1987. A transmission electronmicroscopy study <strong>of</strong> the natural plastic deformation <strong>of</strong>calcic plagioclases (An 68–70). Bulletin de Mineralogie, 110,1–14.OÕBrien, P.J. & Carswell, D.A., 1993. Tectonometamorphicevolution <strong>of</strong> the Bohemian Massif – evidence from highpressuremetamorphic rocks. Geologische Rundschau, 82, 531–555.OÕBrien, P.J. & Ro¨ tzler, J., 2003. High-pressure granulites: formation,recovery <strong>of</strong> peak conditions <strong>and</strong> implications fortectonics. Journal <strong>of</strong> Metamorphic Geology, 21, 3–20.OÕBrien, P.J. & Seifert, K., 1992. P–T–t paths as records <strong>of</strong>orogenic processes: examples <strong>and</strong> problems from the crystalline<strong>of</strong> the Bohemian Massif. Terra Nostra, 1992, 58–59.Passchier, C.W., Trouw, R.A.J., Zwart, H.J. & Vissers, R.L.M.,1992. Porphyroblast rotation – Eppur-Si-Muove. Journal <strong>of</strong>Metamorphic Geology, 10, 283–294.Powell, R. & Holl<strong>and</strong>, T., 1988. An internally consistent datasetwith uncertainties <strong>and</strong> correlations. 3. Applications to geobarometry,worked examples <strong>and</strong> a computer-program.Journal <strong>of</strong> Metamorphic Geology, 6, 173–204.Powell, R. & Holl<strong>and</strong>, T., 2004. Course notes for Ô THERMO-CALC workshop 2004: calculating metamorphic phase equilibriaÕ(ETH Zurich, Switzerl<strong>and</strong>). CD-ROM.Putnis, A., 2002. Mineral replacement reactions: from macroscopicobservations to microscopic mechanisms. MineralogicalMagazine, 66, 689–708.Putnis, A., Pina, C.M., Astilleros, J.M., Fernández-Díaz, L. &Prieto, M., 2003. Nucleation <strong>of</strong> solid solutions crystallisingfrom aqueous solutions. Philosophical Transactions <strong>of</strong> theRoyal Society A: Mathematical, Physical <strong>and</strong> EngineeringSciences, 361, 615–632.Racek, M., Sˇtı´pska´, P., Pitra, P., Schulmann, K. & Lexa, O.,2006. Metamorphic record <strong>of</strong> burial <strong>and</strong> exhumation <strong>of</strong> orogeniclower <strong>and</strong> middle crust: a new tectonothermal model forthe Drosendorf window (Bohemian Massif, Austria). Mineralogy<strong>and</strong> Petrology, 86, 221–251.Ramberg, H., 1952. The Origin <strong>of</strong> Metamorphic <strong>and</strong> MetasomaticRocks. University <strong>of</strong> Chicago Press, Chicago, 317 pp.Ribbe, P.H. (ed.), 1983. Feldspar Mineralogy, 2nd edn. Mineralogicalsociety <strong>of</strong> America, Washington, 362 pp.Rosenberg, C.L. & H<strong>and</strong>y, M.R., 2005. Experimental deformation<strong>of</strong> partially melted granite revisited: implications forthe continental crust. Journal <strong>of</strong> Metamorphic Geology, 23,19–28.Rutter, E.H. & Brodie, K.H., 1988. The role <strong>of</strong> tectonic grainsize reduction in the rheological stratification <strong>of</strong> the lithosphere.Geologische Rundschau, 77, 295–307.Rutter, E.H. & Brodie, K.H., 1992. Rheology <strong>of</strong> the lower crust.In: Continental Lower Crust (eds Fountain, D.M., Arculus, R.& Kay, R.W.), pp. 201–267. Elsevier, Amsterdam.Saheb, N., Boumerzoug, Z., Hamana, D., Laoui, T. & Van DerBiest, O., 1995. Different types <strong>of</strong> discontinuous precipitationin Cu-15 Wt% in alloy. Scripta Metallurgica et Materiala, 32,1453–1458.Sakai, T. & Jonas, J.J., 1984. Dynamic recrystallization:mechanical <strong>and</strong> micro<strong>structural</strong> consideration. Acta Metallurgica,32, 198–209.Schmid, S.M. & Casey, M., 1986. Complete fabric analysis <strong>of</strong>some commonly observed quartz c-axis patterns. In: Mineral<strong>and</strong> Rock Deformation: Laboratory Studies (eds Hobbs, B.E. &Heard, H.C.), pp. 263–286. American Geophysical UnionMonograph, Vol. 36, Washington, DC.Schulmann, K., Kro¨ ner, A., Hegner, E. et al., 2005. Chronologicalconstraints on the pre-orogenic history, burial <strong>and</strong>exhumation <strong>of</strong> deep-seated rocks along the eastern margin <strong>of</strong>the Variscan Orogen, Bohemian Massif, Czech Republic.American Journal <strong>of</strong> Science, 305, 407–448.Schulmann, K., Martelat, J.-E., Ulrich, S., Lexa, O., Sˇtı´pska´, P.& Becker, J.K., 2008. Evolution <strong>of</strong> microstructure <strong>and</strong> melttopology in partially molten granitic mylonite: implicationsfor rheology <strong>of</strong> felsic middle crust. Journal <strong>of</strong> GeophysicalResearch, 113, B10406.Schulmann, K., Konopa´sek, J., Janousˇek, V. et al., 2009. AnAndean type Palaeozoic convergence in the Bohemian Massif.Comptes Rendus – Geoscience, 341, 266–286.Seng, H., 1936. Die Migmatitfrage und der Mechanismusparakristalliner Pragung. Geologische Rundschau, 27, 471–492.Sennour, M., Jouneau, P.H. & Esnouf, C., 2004. TEM <strong>and</strong>EBSD investigation <strong>of</strong> continuous <strong>and</strong> discontinuous precipitation<strong>of</strong> CrN in nitrided pure Fe-Cr alloys. Journal <strong>of</strong>Materials Science, 39, 4521–4531.Sˇtı´pská, P. & Powell, R., 2005. Does ternary feldspar constrainthe metamorphic conditions <strong>of</strong> high-grade metaigneousrocks? Evidence from orthopyroxene granulites,Bohemian Massif. Journal <strong>of</strong> Metamorphic Geology, 23, 627–647.Sˇtı´pská, P., Powell, R., White, R.W. & Baldwin, J.A., 2010.Using calculated chemical potential relationships to accountfor coronas around kyanite: an example from the BohemianMassif. Journal <strong>of</strong> Metamorphic Geology, 28, 97–116.Stu¨ nitz, H., 1998. Syndeformational recrystallization – dynamicor compositionally induced? Contributions to Mineralogy <strong>and</strong>Petrology, 131, 219–236.Stu¨ nitz, H. & Tullis, J., 2001. Weakening <strong>and</strong> strain localizationproduced by syn-deformational reaction <strong>of</strong> plagioclase.International Journal <strong>of</strong> Earth Sciences, 90, 136–148.Stu¨ nitz, H., Fitz Gerald, J.D. & Tullis, J., 2003. Dislocationgeneration, slip systems, <strong>and</strong> dynamic recrystallization inexperimentally deformed plagioclase single crystals. Tectonophysics,372, 215–233.Tajčmanova´, L., Konopa´sek, J. & Schulmann, K., 2006. Thermalevolution <strong>of</strong> the orogenic lower crust during exhumationwithin a thickened Moldanubian root <strong>of</strong> the Variscan belt<strong>of</strong> Central Europe. Journal <strong>of</strong> Metamorphic Geology, 24, 119–134.Tajčmanova´, L., Konopa´sek, J. & Connolly, J.A.D., 2007.Diffusion-controlled development <strong>of</strong> silica-undersaturateddomains in felsic granulites <strong>of</strong> the Bohemian Massif (Variscanbelt <strong>of</strong> Central Europe). Contributions to Mineralogy <strong>and</strong>Petrology, 153, 237–250.Tropper, P., Konzett, J. & Finger, F., 2005. Experimental constraintson the formation <strong>of</strong> high-P ⁄ high-T granulites in theÓ 2010 Blackwell Publishing Ltd367
- 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
- Page 16 and 17:
Foreword 4source and freely availab
- Page 18 and 19:
1. Quantitative analysis of deforma
- Page 20 and 21:
1. Quantitative analysis of deforma
- Page 22 and 23:
1. Quantitative analysis of deforma
- Page 24 and 25:
1. Quantitative analysis of deforma
- Page 26 and 27:
1. Quantitative analysis of deforma
- Page 28 and 29:
1. Quantitative analysis of deforma
- Page 31 and 32:
Chapter 2Mechanisms of lower crusta
- Page 33 and 34:
2. Mechanisms of lower crustal flow
- Page 35 and 36:
2. Mechanisms of lower crustal flow
- Page 37 and 38:
2. Mechanisms of lower crustal flow
- Page 39 and 40:
2. Mechanisms of lower crustal flow
- Page 41 and 42:
Chapter 3Quantitative analyses ofme
- Page 43 and 44:
3. Quantitative analyses of metamor
- Page 45 and 46:
3. Quantitative analyses of metamor
- Page 47 and 48:
3. Quantitative analyses of metamor
- Page 49 and 50:
3. Quantitative analyses of metamor
- Page 51:
3. Quantitative analyses of metamor
- Page 54 and 55:
Bibliography 42Culshaw, N., Beaumon
- Page 56 and 57:
Bibliography 44sources and trigger
- Page 58 and 59:
Bibliography 46Skrzypek, E., Štíp
- Page 61 and 62:
Journal of Structural Geology 23 20
- Page 63 and 64:
J. KonopaÂsek et al. / Journal of
- Page 65 and 66:
J. KonopaÂsek et al. / Journal of
- Page 67 and 68:
J. KonopaÂsek et al. / Journal of
- Page 69 and 70:
J. KonopaÂsek et al. / Journal of
- Page 71 and 72:
J. KonopaÂsek et al. / Journal of
- Page 73 and 74:
J. KonopaÂsek et al. / Journal of
- Page 75 and 76:
J. KonopaÂsek et al. / Journal of
- Page 77 and 78:
J. KonopaÂsek et al. / Journal of
- Page 79 and 80:
J. KonopaÂsek et al. / Journal of
- Page 81 and 82:
JOURNAL OF GEOPHYSICAL RESEARCH, VO
- Page 83 and 84:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 85 and 86:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 87 and 88:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 89 and 90:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 91 and 92:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 93 and 94:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 95:
SCHULMANN ET AL.: STRAIN DISTRIBUTI
- Page 98 and 99:
5 - 2 LEXA ET AL.: COLLISION IN WES
- Page 100 and 101:
5 - 4 LEXA ET AL.: COLLISION IN WES
- Page 102 and 103:
5 - 6 LEXA ET AL.: COLLISION IN WES
- Page 104 and 105:
5 - 8 LEXA ET AL.: COLLISION IN WES
- Page 106 and 107:
5 - 10 LEXA ET AL.: COLLISION IN WE
- Page 108 and 109:
5 - 12 LEXA ET AL.: COLLISION IN WE
- Page 110 and 111:
5 - 14 LEXA ET AL.: COLLISION IN WE
- Page 112 and 113:
5 - 16 LEXA ET AL.: COLLISION IN WE
- Page 114 and 115:
156O. Lexa et al. / Journal of Stru
- Page 116 and 117:
158O. Lexa et al. / Journal of Stru
- Page 118 and 119:
160O. Lexa et al. / Journal of Stru
- Page 121 and 122:
DTD 5ARTICLE IN PRESSJournal of Str
- Page 123 and 124:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 125 and 126:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 127 and 128:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 129 and 130:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 131 and 132:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 133 and 134:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 135 and 136:
Table 1Statistical values of the qu
- Page 137 and 138:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 139 and 140:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 141 and 142:
Table 2Summary of parameters derive
- Page 143 and 144:
DTD 5ARTICLE IN PRESSL. Baratoux et
- Page 145 and 146:
J. metamorphic Geol., 2008, 26, 273
- Page 147 and 148:
EXHUMATION IN LARGE HOT OROGEN 275m
- Page 149 and 150:
Probabi l irequencyProbabi l ireque
- Page 151 and 152:
EXHUMATION IN LARGE HOT OROGEN 279y
- Page 153 and 154:
EXHUMATION IN LARGE HOT OROGEN 281N
- Page 155 and 156:
EXHUMATION IN LARGE HOT OROGEN 283w
- Page 157 and 158:
EXHUMATION IN LARGE HOT OROGEN 285a
- Page 159 and 160:
EXHUMATION IN LARGE HOT OROGEN 287w
- Page 161 and 162:
EXHUMATION IN LARGE HOT OROGEN 289T
- Page 163 and 164:
EXHUMATION IN LARGE HOT OROGEN 291O
- Page 165 and 166:
EXHUMATION IN LARGE HOT OROGEN 293r
- Page 167 and 168:
EXHUMATION IN LARGE HOT OROGEN 295B
- Page 169:
EXHUMATION IN LARGE HOT OROGEN 297R
- Page 172 and 173:
Author's personal copyK. Schulmann
- Page 174 and 175:
Author's personal copyK. Schulmann
- Page 176 and 177:
Author's personal copyK. Schulmann
- Page 178 and 179:
Author's personal copyK. Schulmann
- Page 180 and 181:
Author's personal copyK. Schulmann
- Page 182 and 183:
Author's personal copyK. Schulmann
- Page 184 and 185:
Author's personal copyK. Schulmann
- Page 186 and 187:
Author's personal copyK. Schulmann
- Page 188 and 189:
Author's personal copyK. Schulmann
- Page 190 and 191:
Author's personal copyK. Schulmann
- Page 193 and 194:
J. metamorphic Geol., 2011, 29, 79-
- Page 195 and 196:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 197 and 198:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 199 and 200:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 201 and 202:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 203 and 204:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 205 and 206:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 207 and 208:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 209 and 210:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 211 and 212:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 213 and 214:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 215 and 216:
HEAT SOURCES AND EXHUMATION MECHANI
- Page 217 and 218:
J. metamorphic Geol., 2011, 29, 53-
- Page 219 and 220:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 221 and 222:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 223 and 224:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 225 and 226:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 227 and 228:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 229 and 230:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 231 and 232:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 233 and 234:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 235 and 236:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 237 and 238:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 239 and 240:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 241 and 242:
EXTRUSIONOFLOWERCRUSTINVARISCANOROG
- Page 243 and 244:
J. metamorphic Geol., 2005, 23, 649
- Page 245 and 246:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 247 and 248:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 249 and 250:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 251 and 252:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 253 and 254:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 255 and 256:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 257 and 258:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 259 and 260:
CONTRASTING TEXTURAL RECORD OF TWO
- Page 261 and 262:
Contrasting microstructures and def
- Page 263 and 264:
TEXTURES OF NATURALLY DEFORMED META
- Page 265 and 266:
TEXTURES OF NATURALLY DEFORMED META
- Page 267 and 268:
TEXTURES OF NATURALLY DEFORMED META
- Page 269 and 270:
TEXTURES OF NATURALLY DEFORMED META
- Page 271 and 272:
TEXTURES OF NATURALLY DEFORMED META
- Page 273 and 274:
1.0--0.9__Mg~(Mg2++Fe2+)9 Core of p
- Page 275 and 276:
TEXTURES OF NATURALLY DEFORMED META
- Page 277 and 278:
' ~'-----2~--~----TEXTURES OF NATUR
- Page 279 and 280:
TEXTURES OF NATURALLY DEFORMED META
- Page 281 and 282:
TEXTURES OF NATURALLY DEFORMED META
- Page 283 and 284:
TEXTURES OF NATURALLY DEFORMED META
- Page 285 and 286:
TEXTURES OF NATURALLY DEFORMED META
- Page 287 and 288:
TEXTURES OF NATURALLY DEFORMED META
- Page 289:
TEXTURES OF NATURALLY DEFORMED META
- Page 292 and 293:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 294 and 295:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 296 and 297:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 298 and 299:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 300 and 301:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 302 and 303:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 304 and 305:
B10210ZÁVADA ET AL.: EXTREME DUCTI
- Page 307 and 308:
ClickHereforFullArticleJOURNAL OF G
- Page 309 and 310:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 311 and 312:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 313 and 314:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 315 and 316:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 317 and 318:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 319 and 320:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 321 and 322:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 323 and 324:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 325 and 326:
B10406SCHULMANN ET AL.: RHEOLOGY OF
- Page 327 and 328: J. metamorphic Geol., 2008, 26, 29-
- Page 329 and 330: ORIGIN OF FELSIC MIGMATITES 31Ó 20
- Page 331 and 332: ORIGIN OF FELSIC MIGMATITES 33durin
- Page 333 and 334: ORIGIN OF FELSIC MIGMATITES 35(a)Ty
- Page 335 and 336: ORIGIN OF FELSIC MIGMATITES 37(a)Pl
- Page 337 and 338: ORIGIN OF FELSIC MIGMATITES 39Grain
- Page 339 and 340: ORIGIN OF FELSIC MIGMATITES 41(a)(b
- Page 341 and 342: ORIGIN OF FELSIC MIGMATITES 43(a)(b
- Page 343 and 344: ORIGIN OF FELSIC MIGMATITES 45Fig.
- Page 345 and 346: ORIGIN OF FELSIC MIGMATITES 47produ
- Page 347 and 348: ORIGIN OF FELSIC MIGMATITES 49stron
- Page 349 and 350: ORIGIN OF FELSIC MIGMATITES 51Cmı
- Page 351: ORIGIN OF FELSIC MIGMATITES 53easte
- Page 354 and 355: 104 J. FRANĚK ET AL.in terms of th
- Page 356 and 357: 106 J. FRANĚK ET AL.Fig. 2. Struct
- Page 358 and 359: 108 J. FRANĚK ET AL.(a)perthite po
- Page 360 and 361: 110 J. FRANĚK ET AL.(a)(b)(c) (d)
- Page 362 and 363: 112 J. FRANĚK ET AL.Table 1. Repre
- Page 364 and 365: 114 J. FRANĚK ET AL.at these P-T c
- Page 366 and 367: 116 J. FRANĚK ET AL.(a)(b)Fig. 10.
- Page 368 and 369: 118 J. FRANĚK ET AL.(a)(b)Fig. 11.
- Page 370 and 371: 120 J. FRANĚK ET AL.Table 2. Quant
- Page 372 and 373: 122 J. FRANĚK ET AL.(a)(b)Fig. 15.
- Page 374 and 375: 124 J. FRANĚK ET AL.Fig. 16. Inter
- Page 376 and 377: 126 J. FRANĚK ET AL.development of
- Page 380: 130 J. FRANĚK ET AL.Southern Bohem