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B10210ZÁVADA ET AL.: EXTREME DUCTILITY OF FELDSPAR AGGREGATESB102108.4. Comparative Rheology Between Feldspars andQuartz[47] Experimental studies show that the creep strength offeldspars deformed at dislocation creep is higher than that ofquartz for the entire range of temperature conditions investigated[Shelton and Tullis, 1981; Jaoul et al., 1984; Handy,1994]. This assumption is essential in assessing rheology ofpolyphase rocks with different proportion of weak quartzand ‘‘strong skeleton’’ formed by feldspars in both loadbearingframework and interconnected weak layer microstructures[Handy, 1990, 1994; Schulmann et al., 1996; Ji etal., 2004; Rybacki and Dresen, 2004]. However, change ofdeformation mechanism in feldspars from dislocation todiffusion creep has never been considered in term ofmineral strength contrast between quartz and feldspars.Exceptionally high finite strains of both feldspars surroundingmuch less elongated quartz ribbons shows well thatquartz represents the strong phase according to Handy[1990, 1994] and feldspars form interconnected weaklayers. The explanation is seen in important contributionof dislocation creep accommodated GBS mechanism to thedominant melt-enhanced grain boundary diffusion creepoperative in both feldspars that significantly decreases theirstrength with respect to quartz simultaneously deforming viadislocation creep-controlled recrystallization mechanisms.[48] Acknowledgments. This work has been kindly supported byGrant Agency of the Czech Academy of Sciences (GAAV) projectIAA3111401. J.K. appreciates the financial support of the Ministry ofEducation, Youth and Sports of the Czech Republic through the ScientificCentre ‘‘Advanced Remedial Technologies and Processes’’ (identificationcode 1M0554). We appreciated constructive reviews of P. Bons, J. Weertman,and an anonymous material scientist and editorial handling of J. C. Mutter.This study was also made possible thanks to the ANR project ‘‘LFO inorogens’’ funding as well as to financial support of CNRS (UMR 7516) toOndrej Lexa.ReferencesArzi, A. (1978), Critical phenomena in the rheology of partially meltedrocks, Tectonophysics, 44, 173–184.Baudelet, B., M. C. Dang, and F. Bordeaux (1992), Mechanical behaviourof an aluminium alloy with fusible grain boundaries, Scr. Metall. Mater.,26(4), 573–578.Behrmann, J. H., and D. Mainprice (1987), Deformation mechanisms in ahigh-temperature quartz-feldspar mylonite: evidence for superplastic flowin the lower continental crust, Tectonophysics, 140, 297–305.Berman, R. G. (1990), Mixing properties of Ca-Mg-Fe-Mn garnets, Am.Mineral., 75, 328–344.Bordeaux, F., M. C. Dang, and B. Baudelet (1994), Percolation and damagebehaviour in materials with liquid grain boundaries, J. Mater. Sci., 29,3023–3030.Boullier, A. M., and Z. Gueguen (1975), SP-Mylonites: origin of somemylonites by superplastic flow, Contrib. Mineral. Petrol., 50, 93–104.Brown, M., and T. Rushmer (1997), The role of deformation in the movementof granitic melt: views from the laboratory and the field, in Deformation-EnhancedMelt Segregation and Metamorphic Fluid Transport,Mineral. Soc. Ser., vol. 8, edited by M. Holness, pp. 111 –144, Chapmanand Hall, London.Brown, M. A., M. Brown, W. D. Carlson, and C. Denison (1999), Topologyof syntectonic melt-flow networks in the deep crust: Inferences fromthree-dimensional images of leucosome geometry in migmatites, Am.Mineral., 84, 1793–1818.Čadek, J. (1988), Creep in Metallic Materials, 372 pp., Elsevier, Amsterdam,Netherlands.Connolly, J. A. D. (1990), Multivariable phase-diagrams—An algorithmbased on generalized thermodynamics, Am. J. Sci., 290(6), 666–718.Connolly, J. A. D., and K. Petrini (2002), An automated strategy for calculationof phase diagram sections and retrieval of rock properties as afunction of physical conditions, J. Metamorph. Geol., 20, 697–708.Connolly, J. A. D., M. B. Holness, D. C. Rubie, and T. Rushmer (1997),Reaction-induced microcracking: An experimental investigation of amechanism for enhancing anatectic melt extraction, Geology, 25(7),591–594.Cooper, R. F., and D. L. Kohlstedt (1984), Solution-precipitation-enhanceddiffusional creep of partially molten olivine-basalt aggregates during hotpressing,Tectonophysics, 107(3–4), 207–233.Cosgrove, J. W. (1997), The influence of mechanical anisotropy on thebehaviour of the lower crust, Tectonophysics, 280(1–2), 1 –14.Daines, M. J., and D. L. Kohlstedt (1997), Influence of deformation on melttopology in peridotites, J. Geophys. Res., 102, 10,257–10,271.Dell’Angelo, L. N., and J. Tullis (1988), Experimental deformation of partiallymelted granitic aggregates, J. Metamorph. Geol., 6(4), 495–515.Dell’Angelo, L. N., J. Tullis, and R. A. Yund (1987), Transition fromdislocation creep to melt-enhanced diffusion creep in fine-grained graniticaggregates, Tectonophysics, 139(3–4), 325–332.Flinn, D. (1962), On folding during three-dimensional progressive deformation,Q. J. Geol. Soc. London, 118, 385–433.Franke, W. (2000), The mid-European segment of the Variscides: tectonostratigraphicunits, terrane boundaries and plate tectonic evolution, inOrogenic Processes: Quantification and Modelling in the Variscan Belt,edited by W. Franke et al., Geol. Soc. Spec. Publ., 179, 35–61.Gabriel, A., and E. P. Cox (1929), A staining method for the quantitativedetermination of certain rock minerals, Am. Mineral., 14, 290–292.Gleason, G. C., V. Bruce, and H. W. Green (1999), Experimental investigationof melt topology in partially molten quartzo-feldspathic aggregatesunder hydrostatic and non-hydrostatic stress, J. Metamorph. Geol., 17,705–722.Gower, R. J. W., and C. Simpson (1992), Phase-boundary mobility innaturally deformed, high-grade quartzo-feldspathic rocks—Evidence fordiffusional creep, J. Struct. Geol., 14, 301–313.Handy, M. R. (1990), The solid-state flow of polymineralic rocks, J. Geophys.Res., 95, 8647–8661.Handy, M. R. (1994), Flow laws for rocks containing 2 nonlinear viscousphases—A phenomenological approach, J. Struct. Geol., 16, 287–301.Hanmer, S. (1982), Microstructure and geochemistry of plagioclase andmicrocline in naturally deformed granite, J. Struct. Geol., 4, 232.Hirth, G., and J. Tullis (1992), Dislocation creep regimes in quartz aggregates,J. Struct. Geol., 14, 145–159.Holland, T. J. B., and R. Powell (1998), An internally consistent thermodynamicdata set for phases of petrological interest, J. Metamorph. Geol.,16(3), 309–343.Hollister, L. S., and M. L. Crawford (1986), Melt-enhanced deformation—A major tectonic process, Geology, 14(7), 558–561.Holtzman, B. K., N. J. Groebner, M. E. Zimmerman, S. B. Ginsberg, andD. L. Kohlstedt (2003), Stress-driven melt segregation in partially moltenrocks, Geochem. Geophys. Geosyst., 4(5), 8607, doi:10.1029/2001GC000258.Holyoke, C. W., and T. Rushmer (2002), An experimental study of grainscale melt segregation mechanisms in two common crustal rock types,J. Metamorph. Geol., 20(5), 493–512.Hradecký, P. (Ed.) (2002), Geological map 1:25000, Map 11-221. CzechGeol. Surv., Prague, Czech Republic.Hubbert, M. K., and W. W. Rubey (1959), Role of fluid pressure in mechanicsof overthrust faulting, Geol. Soc. Am. Bull., 70, 116–166.Jaoul, O., J. Tullis, and A. Kronenberg (1984), The effect of varying watercontent on the behaviour of Heavitree quartzite, J. Geophys. Res., 89,4298–4312.Jessell, M. W. (1987), Grain boundary migration microstructures in a naturallydeformed quartzite, J. Struct. Geol., 9, 1007–1014.Ji, S. C., Z. T. Jiang, E. Rybacki, R. Wirth, D. Prior, and B. Xia (2004),Strain softening and microstructural evolution of anorthite aggregates andquartz-anorthite layered composites deformed in torsion, Earth Planet.Sci. Lett., 222(2), 377–390.Jurewicz, S. R., and E. B. Watson (1984), Distribution of partial melt in afelsic system - the importance of surface energy, Contrib. Mineral. Petrol.,85(1), 25–29.Kassner, M. E., and T. A. Hayes (2003), Creep cavitation in metals, Int. J.Plasticity, 19(10), 1715–1748.Koike, J., K. Miki, K. Maruyama, and H. Oikawa (1998), Effects of theliquid phase on the high-temperature tensile ductility: from embrittlementto superplasticity, Philos. Mag. A, 3, 599–614.Konopásek, J., and K. Schulmann (2005), Contrasting Early Carboniferousfield geotherms: Evidence for accretion of a thickened orogenic root andsubducted Saxothuringian crust (central European Variscides), J. Geol.Soc., 162, 463–470.Konopásek, J., K. Schulmann, and O. Lexa (2001), Structural evolution ofthe central part of the Krušné hory (Erzgebirge) Mountains in the CzechRepublic—Evidence for changing stress regime during Variscan compression,J. Struct. Geol., 23, 1373–1392.Kotková, J., A. Kröner, W. Todt, and J. Fiala (1996), Zircon dating of northBohemian granulites, Czech Republic: Further evidence for the Lower14 of 15292
B10210ZÁVADA ET AL.: EXTREME DUCTILITY OF FELDSPAR AGGREGATESB10210Carboniferous high-pressure event in the Bohemian Massif, Geol.Rundsch., 85(1), 154–161.Kretz, R. (1983), Symbols for rock-forming minerals, Am. Mineral., 68,277–279.Kruse, R., H. Stünitz, and A. Kunze (2001), Dynamic recrystallizationprocesses in plagioclase porphyroclasts, J. Struct. Geol., 23, 1781–1802.Langdon, T. G., and R. B. Vastava (1982), An evaluation of deformationmodels for grain boundary sliding, in Mechanical Testing for DeformationModel Development, edited by R. W. Rohde and J. C. Swearengen,Am. Soc. for Test. of Mater., Philadelphia, Pa.Lexa, O., P. Štípská, K. Schulmann, L. Baratoux, and A. Kröner (2005), Contrastingtextural record of two distinct metamorphic events of similar P-Tconditions and different durations, J. Metamorph. Geol., 23(8), 649–666.Lister, G. S., and U. F. Dornsiepen (1982), Fabric transitions in the Saxonygranulite terrain, J. Struct. Geol., 4, 81–92.Lister, G. S., and B. E. Hobbs (1980), The simulation of fabric developmentduring plastic deformation and its application to quartzite: The influenceof deformation history, J. Struct. Geol., 2, 355–370.Mabuchi, M., H. G. Jeong, K. Hiraga, and K. Higashi (1997), Partialmelting at interfaces and grain boundaries for high-strain-rate superplasticmaterials, Interface Sci., 4(3–4), 357–368.Marchildon, N., and M. Brown (2001), Melt segregation in late syn-tectonicanatectic migmatites: An example from the Onawa contact aureole,Maine, USA, Phys. Chem. Earth, Part A, 26(4–5), 225–229.Marshall, D. B., and A. C. McLaren (1977), Deformation mechanisms inexperimentally deformed plagioclase feldspars, Phys. Chem. Mineral., 1,351–370.Martelat, J. E., K. Schulmann, J. M. Lardeaux, C. Nicollet, and H. Cardon(1999), Granulite microfabrics and deformation mechanisms in southernMadagascar, J. Struct. Geol., 21, 671–687.McKenzie, D. (1984), The generation and compaction of partially moltenrock, J. Petrol., 25(3), 713–765.Mehnert, K. R., W. Busch, and G. Schneider (1973), Initial melting at grainboundaries of quartz and feldspar in gneisses and granulites, Neues Jahb.Mineral., 4, 165–183.Mohamed, F. A. (2002), The role of impurities during creep and superplasticityat very low stresses, Metall. Mater. Trans. A., 33, 261–278.Morgan, S. S., and R. D. Law (2004), Unusual transition in quartzite dislocationcreep regimes and crystal slip systems in the aureole of theEureka Valley-Joshua Flat-Beer Creek pluton, California: a case for anhydrousconditions created by decarbonation reactions, Tectonophysics,384(1–4), 209–231.Newton, R. C., T. V. Charlu, and O. J. Kleppa (1980), Thermochemistry of highstructural state plagioclases, Geochim. Cosmochim. Acta, 44, 933–941.Olsen, T. S., and D. L. Kohlstedt (1984), Analysis of dislocations in somenaturally deformed plagioclase feldspars, Phys. Earth Planet. Inter., 11,153–160.Passchier, C. W., and R. A. J. Trouw (1996), Microtectonics, 325pp.,Springer Verlag, Berlin.Pharr, G. M., P. S. Godavarti, and B. L. Vaandrager (1989), Effects ofwetting on the compression creep behaviour of metals containing lowmelting intergranular phases, J. Mater. Sci., 24, 784–792.Poirier, J. P. (1985), Creep of Crystals, 260 pp., Cambridge Univ. Press,Cambridge, U.K.Powell, R., and T. J.B. Holland (1999), Relating formulations of the thermodynamicsof mineral solid solutions; activity modeling of pyroxenes,amphiboles and micas, Am. Mineral., 84, 1–14.Price, N. J., and J. W. Cosgrove (1990), Analysis of Geological Structures,502 pp, Cambridge Univ. Press, Cambridge, U.K.Ramsay, J. G., and M. I. Huber (1983), The Techniques of Modern StructuralGeology, vol. 1, 307 pp., Academic, London.Ranalli, G. (1995), Rheology of the Earth, 2nd ed., 413 pp., Chapmann andHall, New York.Renner, J., B. Evans, and G. Hirth (2000), On the rheologically critical meltfraction, Earth Planet. Sci. Lett., 181(4), 585–594.Rosenberg, C. L. (2001), Deformation of partially molten granite: A reviewand comparison of experimental and natural case studies, Int. J. EarthSci., 90(1), 60–76.Rosenberg, C. L., and M. R. Handy (2000), Syntectonic melt pathways duringsimple shearing of a partially molten rock analogue (Norcamphor-Benzamide), J. Geophys. Res., 105, 3135– 3149.Rosenberg, C. L., and M. R. Handy (2005), Experimental deformationof partially melted granite revisited: implications for the continental crust,J. Metamorph. Geol., 23(1), 19–28.Rosenberg, C. L., and U. Riller (2000), Partial-melt topology in staticallyand dynamically recrystallized granite, Geology, 28(1), 7–10.Rushmer, T. (1996), Melt segregation in the lower crust: How have experimentshelped us?, Trans. R. Soc. Edinburgh Earth Sci., 87(1–2),73–83.Rushmer, T. (2001), Volume change during partial melting reactions: implicationsfor melt extraction, melt geochemistry and crustal rheology,Tectonophysics, 342(3–4), 389–405.Rutter, E. H., and D. H. K. Neumann (1995), Experimental deformation ofpartially molten Westerly granite under fluid-absent conditions, with implicationsfor the extraction of granitic magmas, J. Geophys. Res., 100,15,697–15,715.Rybacki, E., and G. Dresen (2004), Deformation mechanism maps forfeldspar rocks, Tectonophysics, 382(3–4), 173–187.Sawyer, E. W. (2001), Melt segregation in the continental crust: Distributionand movement of melt in anatectic rocks, J. Metamorph. Geol.,19(3), 291–309.Schmid, S. M., R. Heilbronner, and H. Stünitz (1999), Deformation mechanismsin nature and experiment, Tectonophysics, 303(1–4), vii –ix.Schulmann, K., R. Melka, and B. Mlčoch (1996), High-temperature microstructuresand rheology of deformed granite, Erzgebirge, Bohemian Massif,J. Struct. Geol., 18, 719–733.Shelton, G., and J. Tullis (1981), Experimental flow laws for crustal rocks,Eos Trans. AGU, 62, 396.Sklenička, V., I. Saxl, and J. Čadek (1977), Mezikrystalový lom při VysokoteplotnímCreepu Kovù a Slitin (Intercrystalline Fracturing at HighTemperature Creep of Metals and Alloys), 108 pp., ČSAV, Prague.Smith, J. V. (1974), Feldspar Minerals. 1. Crystal Structure and PhysicalProperties, 627 pp., Springer, Berlin.Spry, A. (1969), Metamorphic Textures, 350 pp., Pergamon, Oxford, U.K.Thompson, J. B., and G. L. Hovis (1979), Entropy of mixing in sanidine,Am. Mineral., 64, 57–65.Tullis, J. (1983), Deformation of feldspars, in Feldspar Mineralogy, Rev.Mineral., vol. 2, edited by P. H. Ribbe, pp. 297–323, Mineral. Soc. ofAm., Washington, D. C.Tullis, J., and R. A. Yund (1991), Diffusion creep in feldspar aggregates—Experimental-evidence, J. Struct. Geol., 13, 987–1000.Ulrich, S., K. Schulmann, and M. Casey (2002), Microstructural evolutionand rheological behaviour of marbles deformed at different crustal levels,J. Struct. Geol., 24, 979–995.van der Molen, I., and M. S. Paterson (1979), Experimental deformation ofpartially-melted granite, Contrib. Mineral. Petrol., 70, 299–318.Vigneresse, J. L., P. Barbey, and M. Cuney (1996), Rheological transitionsduring partial melting and crystallization with application to felsicmagma segregation and transfer, J. Petrol., 37(6), 1579–1600.Vollbrecht, A., M. Stipp, and N. Ø. Olesen (1999), Crystallographic orientationof microcracks in quartz and inferred deformation processes: Astudy on gneisses from the German Continental Deep Drilling Project(KTB), Tectonophysics, 303(1–4), 279–297.Wadsworth, J., O. A. Ruano, and O. D. Sherby (1999), Deformation bygrain boundary sliding and slip creep versus diffusional creep, paperpresented at the Minerals, Metal and Materials Society Annual Meeting,San Diego, Calif.Walte, N. P., P. D. Bons, and C. W. Passchier (2005), Deformation of meltbearingsystem-insight from in situ grain-scale analogue experiments,J. Struct. Geol., 27, 1666–1679.Wei, Y. H., Q. D. Wang, Y. P. Zhu, H. T. Zhou, W. J. Ding, Y. Chino, andM. Mabuchi (2003), Superplasticity and grain boundary sliding in rolledAZ91 magnesium alloy at high strain rates, Mater. Sci. Eng. A, 360, 107–115.White, R. W., R. Powell, and T. J. B. Holland (2001), Calculation of 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(2), 139–153.Willaime, C., and M. Gandais (1977), Electron microscope study of plasticdefects in experimentally deformed alkali feldspars, Bull. Soc. Fr.Mineral. Cristall., 100(5), 263–271.Willaime, C., J. M. Christie, and D. Mainprice (1979), Experimental deformationof K-feldspar single crystals, Bull. Mineral., 102, 168–177.Zhang, Y., B. E. Hobbs, and M. W. Jessell (1994), The effect of grainboundarysliding on fabric development in polycrystalline aggregates,J. Struct. Geol., 16, 1315–1325.Zulauf, G., W. Dörr, J. Fiala, J. Kotková, H. Maluski, and P. Valverde-Vaquero (2002), Evidence for high-temperature diffusional creep preservedby rapid cooling of lower crust (North Bohemian shear zone,Czech Republic), Terra Nova, 14(5), 343–354.J. Konopásek, Czech Geological Survey, Prague, Czech Republic.(konopasek@cgu.cz)O. Lexa and K. Schulmann, Centre de Geochimie de la Surface, UMR7516, Université Louis Pasteur, Strasbourg, 67000 Cedex, France.(lexa@illite.u-strasbg.fr; schulman@illite.u-strasbg.fr)S. Ulrich, Geophysical Institute, Czech Academy of Sciences, Prague,Czech Republic. (stano@ig.cas.cz)P. Závada, Institute of Petrology and Structural Geology, CharlesUniversity, Prague, Czech Republic. (zavada@natur.cuni.cz)15 of 15293
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Contentsviii4.7 Schulmann, Konopás
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Dedicated to my wife Markéta, daug
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Foreword 2First topic “Quantitati
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Foreword 4source and freely availab
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1. Quantitative analysis of deforma
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Chapter 2Mechanisms of lower crusta
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2. Mechanisms of lower crustal flow
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Chapter 3Quantitative analyses ofme
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3. Quantitative analyses of metamor
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Bibliography 42Culshaw, N., Beaumon
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Bibliography 44sources and trigger
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Bibliography 46Skrzypek, E., Štíp
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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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