B10406SCHULMANN ET AL.: RHEOLOGY OF PARTIALLY MOLTEN GNEISSESB10406J. Metamorph. Geol., 23, 19– 28, doi:10.1111/j.1525-1314.2005.00555.x.Rybacki, E., <strong>and</strong> G. Dresen (2004), Deformation mechanism mapsfor feldspar rocks, Tectonophysics, 382, 173–187, doi:10.1016/j.tecto.2004.01.006.Sawyer, E. W. (2001), Melt segregation in the continental crust: Distribution<strong>and</strong> movement <strong>of</strong> melt in anatectic rocks, J. Metamorph. Geol., 19,291–309, doi:10.1046/j.0263-4929.2000.00312.x.Scaillet, B., C. France-Lanord, <strong>and</strong> P. Le Fort (1990), Badrinath-Gangotriplutons (Garhwal, India): Petrological <strong>and</strong> geochemical evidence for fractionationprocesses in a high Himalayan leucogranite, J. Volcanol.Geotherm. Res., 44, 163–188, doi:10.1016/0377-0273(90)90017-A.Schmid, S. M. (1982), Micr<strong>of</strong>abric studies as indicators <strong>of</strong> deformationmechanisms <strong>and</strong> flow laws operative in mountain building, in MountainBuilding Processes, edited by K. J. Hsü, pp. 95–110, Elsevier, London.Schmid, S. M., <strong>and</strong> M. Casey (1986), Complete fabric analysis <strong>of</strong> somecommonly observed quartz c-axis patterns, in Mineral <strong>and</strong> Rock Deformation:Laboratory Studies, Geophys. Monogr. Ser., vol. 36, edited byB. E. Hobbs <strong>and</strong> H. C. Heard, pp. 263–286, AGU, Washington, D. C.Schmid, S. M., R. Panozzo, <strong>and</strong> S. Bauer (1987), Simple shear experimentson calcite rocks: Rheology <strong>and</strong> micr<strong>of</strong>abric, J. Struct. Geol., 9, 747–778,doi:10.1016/0191-8141(87)90157-X.Schmid, S. M., R. Heilbronner, <strong>and</strong> H. Stünitz (1999), Deformation mechanismsin nature <strong>and</strong> experiment (editorial remarks), Tectonophysics,303, vii–ix, doi:10.1016/S0040-1951(98)00302-3.Schulmann, K., B. Mlcoch, <strong>and</strong> R. Melka (1996), High-temperature microstructures<strong>and</strong> rheology <strong>of</strong> deformed granite, Erzgebirge, Bohemian Massif,J. Struct. Geol., 18, 719–733, doi:10.1016/S0191-8141(96)80007-1.Schulmann, K., A. Kröner, E. Hegner, I. Wendt, J. Konopásek, O. Lexa,<strong>and</strong> P. Štípská (2005), Chronological constraints on the pre-orogenichistory, burial <strong>and</strong> exhumation <strong>of</strong> deep-seated rocks along the easternmargin <strong>of</strong> the Variscan Orogen, Bohemian Massif, Czech Republic,Am. J. Sci., 305, 407–448, doi:10.2475/ajs.305.5.407.Simpson, C. (1985), Deformation <strong>of</strong> granitic rocks across the brittle-ductiletransition, J. Struct. Geol., 7, 503–511, doi:10.1016/0191-8141(85)90023-9.Sklenička, V., J. Saxl, <strong>and</strong> J. Čadek (1977), Intercrystalline fracturing athigh temperature creep <strong>of</strong> metals <strong>and</strong> alloys (in Czech), report, 108 pp.,Czech. Acad. <strong>of</strong> Sci., Prague.Stünitz, H., <strong>and</strong> J. D. Fitz Gerald (1993), Deformation <strong>of</strong> granitoids at lowmetamorphic grades. II. Granular flow in albite-rich mylonites, Tectonophysics,221, 299–324, doi:10.1016/0040-1951(93)90164-F.Synek, J., <strong>and</strong> D. Oliverová (1993), Terrane character <strong>of</strong> the north-eastmargin <strong>of</strong> the Moldanubian Zone: The Kutná Hora Crystalline Complex,Bohemian Massif, Geol. Rundsch., 82, 566 –582, doi:10.1007/BF00212417.Tajcmanová, L., J. Konopásek, <strong>and</strong> K. Schulmann (2006), Thermal evolution<strong>of</strong> the orogenic lower crust during exhumation within a thickenedMoldanubian root <strong>of</strong> the Variscan belt <strong>of</strong> Central Europe, J. Metamorph.Geol., 24, 119–134, doi:10.1111/j.1525-1314.2006.00629.x.Tharp, T. M. (1983), Analogies between the high-temperature deformation<strong>of</strong> polyphase rocks <strong>and</strong> the mechanical behavior <strong>of</strong> porous powder metal,Tectonophysics, 96, 1–11, doi:10.1016/0040-1951(83)90216-0.Thompson, A. B., <strong>and</strong> J. A. D. Connolly (1995), Melting <strong>of</strong> the continentalcrust: Some thermal <strong>and</strong> petrological constraints on anatexis in continentalcollision zones <strong>and</strong> other tectonic settings, J. Geophys. Res., 100,15,565–15,580, doi:10.1029/95JB00191.Treagus, S. H. (2002), Modelling the bulk vicosity <strong>of</strong> two-phase mixtures interm <strong>of</strong> clast shape, J. Struct. Geol., 24, 57 – 76, doi:10.1016/S0191-8141(01)00049-9.Tullis, J. (1983), Deformation <strong>of</strong> feldspars, in Feldspar Mineralogy, Rev.Mineral., vol. 2, 2nd ed., edited by P. H. Ribbe, pp. 297–323, Mineral.Soc. <strong>of</strong> Am., Washington, D. C..Tullis, J. (1990), Experimental studies <strong>of</strong> deformation mechanisms <strong>and</strong>microstructures in quartzo-feldspathic rocks, in Deformation Processesin Minerals, Ceramics <strong>and</strong> Rocks, edited by D. Barbour <strong>and</strong> P. Meredith,pp.190–227, CRC Press, Cambridge, U. K.Walte, N. P., P. D. Bons, <strong>and</strong> C. W. Passchier (2005), Deformation <strong>of</strong> meltbearingsystems — Insight from in situ grain-scale analogue experiments,J. Struct. Geol., 27, 1666–1679, doi:10.1016/j.jsg.2005.05.006.White, J. C., <strong>and</strong> C. K. Mawer (1986), Extreme ductility <strong>of</strong> feldspars from amylonite, Parry Sound, Canada, J. Struct. Geol., 8, 133 –143,doi:10.1016/0191-8141(86)90104-5.White, J. C., <strong>and</strong> C. K. Mawer (1988), Dynamic recrystallization <strong>and</strong>associated in perthites: Evidence <strong>of</strong> deep crustal thrusting, J. Geophys.Res., 93, 325–337, doi:10.1029/JB093iB01p00325.White, R. W., R. Powell, <strong>and</strong> T. J. B. Holl<strong>and</strong> (2001), Calculation <strong>of</strong> partialmelting equilibria in the system Na 2 O–CaO–K 2 O–FeO–MgO–Al 2 O 3 –SiO 2 –H 2 O (NCKFMASH), J. Metamorph. Geol., 19, 139–153, doi:10.1046/j.0263-4929.2000.00303.x.Závada, P., K. Schulmann, J. Konopásek, O. Lexa, <strong>and</strong> S. Ulrich (2007),Melt topology in deformed quartzo-feldspathic rocks: Implicationfor rheology <strong>and</strong> grain-scale migration <strong>of</strong> melt in partially molten crust,J. Geophys. Res., 112, B10210, doi:10.1029/2006JB004820.J. K. Becker, Institut für Geowissenschaften, Universität Tübingen,Sigwartstrasse 10, D-72076 Tübingen, Germany.O. Lexa, Institute <strong>of</strong> Petrology <strong>and</strong> Structural Geology, CharlesUniversity, Albertov 6, 12843 Praha 2, Czech Republic.J.-E. Martelat, Laboratoire de Géodynamique des Chaînes Alpines,UMR5025, Université Joseph Fourier, Observatoire des Sciences del’Univers de Grenoble, CNRS, F-38041 Grenoble Cedex 9, France.K. Schulmann <strong>and</strong> P. Štípská, Centre de Géochimie de la Surface,UMR7516, Université Louis Pasteur, CNRS, F-67084 Strasbourg Cedex,France.S. Ulrich, Geophysical Institute, Czech Academy <strong>of</strong> Sciences, Boční II/1401, 14131 Praha 4, Czech Republic.20 <strong>of</strong> 20314
J. metamorphic Geol., 2008, 26, 29–53 doi:10.1111/j.1525-1314.2007.00743.xOrigin <strong>of</strong> migmatites by deformation-enhanced melt infiltration<strong>of</strong> orthogneiss: a new model based on quantitativemicro<strong>structural</strong> analysisP. HASALOVÁ, 1,2 K. SCHULMANN, 1 O. LEXA, 1,2 P. ŠTÍPSKÁ, 1 F. HROUDA, 2,3 S. ULRICH, 2,4J. HALODA 5 AND P. TÝCOVÁ 51 Université Louis Pasteur, CGS/EOST, UMR 7517, 1 rue Blessig, Strasbourg 67084, France (hasalovap@seznam.cz)2 Institute <strong>of</strong> Petrology <strong>and</strong> Structural Geology, Charles University, Albertov 6, 12843 Prague, Czech Republic3 AGICO, Ječná 29a, 621 00 Brno, Czech Republic4 Institute <strong>of</strong> Geophysics, Czech Academy <strong>of</strong> Sciences, Boční II/1401, 14131 Praha 4, Czech Republic5 Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech RepublicABSTRACTA detailed field study reveals a gradual transition from high-grade solid-state b<strong>and</strong>ed orthogneiss viastromatic migmatite <strong>and</strong> schlieren migmatite to irregular, foliation-parallel bodies <strong>of</strong> nebulitic migmatitewithin the eastern part <strong>of</strong> the Gfo¨ hl Unit (Moldanubian domain, Bohemian Massif). The orthogneiss tonebulitic migmatite sequence is characterized by progressive destruction <strong>of</strong> well-equilibrated b<strong>and</strong>edmicrostructure by crystallization <strong>of</strong> new interstitial phases (Kfs, Pl <strong>and</strong> Qtz) along feldspar boundaries<strong>and</strong> by resorption <strong>of</strong> relict feldspar <strong>and</strong> biotite. The grain size <strong>of</strong> all felsic phases decreases continuously,whereas the population density <strong>of</strong> new phases increases. The new phases preferentially nucleate alonghigh-energy like–like boundaries causing the development <strong>of</strong> a regular distribution <strong>of</strong> individual phases.This evolutionary trend is accompanied by a decrease in grain shape preferred orientation <strong>of</strong> all felsicphases. To explain these data, a new petrogenetic model is proposed for the origin <strong>of</strong> felsic migmatites bymelt infiltration from an external source into b<strong>and</strong>ed orthogneiss during deformation. In this model,infiltrating melt passes pervasively along grain boundaries through the whole-rock volume <strong>and</strong> changescompletely its macro- <strong>and</strong> microscopic appearance. It is suggested that the individual migmatite typesrepresent different degrees <strong>of</strong> equilibration between the host rock <strong>and</strong> migrating melt duringexhumation. The melt topology mimicked by feldspar in b<strong>and</strong>ed orthogneiss forms elongate pocketsoriented at a high angle to the compositional b<strong>and</strong>ing, indicating that the melt distribution wascontrolled by the deformation <strong>of</strong> the solid framework. The microstructure exhibits features compatiblewith a combination <strong>of</strong> dislocation creep <strong>and</strong> grain boundary sliding deformation mechanisms. Themigmatite microstructures developed by granular flow accompanied by melt-enhanced diffusion <strong>and</strong>/ormelt flow. However, an AMS study <strong>and</strong> quartz micr<strong>of</strong>abrics suggest that the amount <strong>of</strong> melt present didnot exceed a critical threshold during the deformation to allow free movements <strong>of</strong> grains.Key words: crystal size distribution; melt infiltration; melt topology; migmatites; quantitative texturalanalysis.INTRODUCTIONMovement <strong>of</strong> a large volume <strong>of</strong> granitic melt is animportant factor in the compositional differentiation<strong>of</strong> the continental crust (Fyfe, 1973; Collins & Sawyer,1996; Brown & Rushmer, 2006) <strong>and</strong> the presence <strong>of</strong>melt in rocks pr<strong>of</strong>oundly influences their rheology(Arzi, 1978). The migration <strong>of</strong> melt through the crust iscontrolled by melt buoyancy <strong>and</strong> pressure gradientsresulting from the combination <strong>of</strong> gravity forces <strong>and</strong>deformation (Wickham, 1987; Sawyer, 1994). Thereare three major mechanisms controlling melt migrationthrough the continental crust: (i) diapirism resulting inupward motion <strong>of</strong> low-density magma through higherdensity rocks (Ch<strong>and</strong>rasekhar, 1961; Ramberg, 1981);(ii) dyking that describes melt migration by hydr<strong>of</strong>racturing<strong>of</strong> the host rock <strong>and</strong> transport <strong>of</strong> meltthrough narrow dykes (Lister & Kerr, 1991; Petford,1995); (iii) <strong>and</strong> migration <strong>of</strong> a melt through a network<strong>of</strong> interconnected pores during deformation or compaction<strong>of</strong> solid matrix (McKenzie, 1984; Wickham,1987).Brown & Solar (1998a) <strong>and</strong> Weinberg & Searle(1998) proposed that during active deformation meltmoves by pervasive flow <strong>and</strong> it is essentially pumpedthrough the system parallel to the principal finiteelongation in the form <strong>of</strong> foliation-parallel veins.Based on a number <strong>of</strong> field studies, pervasive meltmigration at outcrop scale controlled by regionaldeformation has been suggested by various authors(Collins & Sawyer, 1996; Brown & Solar, 1998b;V<strong>and</strong>erhaeghe, 1999; Marchildon & Brown, 2003).Ó 2007 Blackwell Publishing Ltd 29315
- 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: B10406SCHULMANN ET AL.: RHEOLOGY OF
- 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 378 and 379:
128 J. FRANĚK ET AL.Behrmann, J.H.
- Page 380:
130 J. FRANĚK ET AL.Southern Bohem
Change language