Abstract
The Barrovian inverted metamorphism of the Svratka dome developed within two nappes derived from the Brunia continent that was thrust beneath the Moldanubian orogenic root. The metamorphism increases from biotite–chlorite zone in the basement to very closely spaced staurolite, kyanite and sillimanite zones at the top of the nappe pile. The sequence of mineral growth, chemical zoning of garnet, and pseudosection modelling indicate prograde paths from 4.5 kbar/510 °C to 5.5 kbar/540 °C in the garnet zone, from 6 kbar/530 °C to 7 kbar/600 °C in the staurolite zone, and from 3.5 kbar/510 °C to 8.5 kbar/650 °C in the kyanite zone. The age of monazite inclusions in garnet and staurolite is interpreted to reflect prograde metamorphism at 338 ± 7 Ma and 336 ± 7 Ma, respectively. An older matrix monazite crystal is interpreted as dating prograde crystallization at 345 ± 7 Ma, whereas a younger monazite group records recrystallization at/or down to 334 ± 7 Ma. While these petrological and geochronological data are consistent with data from an inverted metamorphic sequence of the southern Thaya dome, the spacing and distribution of metamorphic zones, nappe thicknesses, and late structures are different in the two domes. An antiformal stack of imbricated basement sheets and the extreme attenuation of metamorphic isograds at the top of the nappe pile in the Svratka dome are explained by a relatively cold overthrusting Moldanubian domain, formed mainly of middle orogenic crust. The homogeneous thickening of the hinterland-dipping basement duplexes and the regular spacing of metamorphic isograds in the Thaya dome are explained by a hot overriding Moldanubian domain, which in this region has a high proportion of exhumed lower orogenic crust and formed a hot mid-crustal channel.
This is a preview of subscription content, log in via an institution to check access.
Similar content being viewed by others
References
Aleinikoff JN, Schenck WS, Plank MO, Srogi LA, Fanning CM, Kamo SL, Bosbyshell H (2006) Deciphering igneous and metamorphic events in high-grade rocks of the Wilmington complex, Delaware: morphology, cathodoluminescence and backscattered electron zoning, and SHRIMP U-Pb geochronology of zircon and monazite. Bull Geol Soc Am 118:39–64. https://doi.org/10.1130/B25659.1
Arita K (1983) Origin of the inverted metamorphism of the lower Himalayas, Central Nepal. Tectonophysics 95:43–60. https://doi.org/10.1016/0040-1951(83)90258-5
Barcheck CG, Wiens DA, van Keken PE, Hacker BR (2012) The relationship of intermediate- and deep-focus seismicity to the hydration and dehydration of subducting slabs. Earth Plan Sci Lett 349–350:153–160. https://doi.org/10.1016/j.epsl.2012.06.055
Bea F, Montero P (1999) Behavior of accessory phases and redistribution of Zr, REE, Y, Th, and U during metamorphism and partial melting of metapelites in the lower crust: an example from the Kinzigite Formation of Ivrea-Verbano, NW Italy. Geochim Cosmochim Acta 63:1133–1153. https://doi.org/10.1016/S0016-7037(98),00292-0
Boyer SE, Elliott D (1982) Thrust systems. Am Asso Petrol Geol Bull 66:1196–1230
Broussolle A, Štípská P, Lehmann J, Schulmann K, Hacker BR, Holder R, Kylander-Clark ARC, Hanžl P, Racek M, Hasalová P, Lexa O, Hrdličková K, Buriánek D (2015) P-T–t–D record of crustal-scale horizontal flow and magma-assisted doming in the SW Mongolian Altai. J Metamorph Geol 33:359–383. https://doi.org/10.1111/jmg.12124
Brunel M, Kienast JR (1986) Etude petro-structurale des chevauchements ductiles himalayens sur la transversal de l’Everest-Makalu (Nepal oriental). 23:1117–1137. https://doi.org/10.1139/e86-111
Burg JP, Leyreloup A, Marchand J, Matte P (1984) Inverted metamorphic zonation and large-scale thrusting in the Variscan Belt: an example in the French Massif Central, pp 47–61
Burg JP, Delor CP, Leyreloup AF, Romney F (1989) Inverted metamorphic zonation and Variscan thrust tectonics in the Rouergue area (Massif Central, France): P–T–t record from mineral to regional scale. In: Daly JS, Cliff RA, Yardley BWD (eds) Evolution of Metamorphic Belts, vol 43. Geological Society Special Publication. pp 423–439
Buriánek D, Hrdličková K, Hanžl P (2009) Geological position and origin of augen gneisses from the Polička Unit, eastern Bohemian Massif. J Geosci 54:201–219. https://doi.org/10.3190/jgeosci.043
Coggon R, Holland TJB (2002) Mixing properties of phengitic micas and revised garnet-phengite thermobarometers. J Metamorph Geol 20:683–696. https://doi.org/10.1046/j.1525-1314.2002.00395.x
Compston W, Williams IS, Kirschvink JL, Zhang Z, Ma G (1992) Zircon U–Pb ages for the early Cambrian time-scale. J Geol Soc 149:171–184. https://doi.org/10.1144/gsjgs.149.2.0171
Dallmeyer D, Neubauer F, Höck V (1992) 40Ar/39Ar mineral age controls on the chronology of late- Paleozoic tectonothermal activity in the southeastern Bohemian Massif. Austria (Moldanubian and Moravosilesian zone). 210:135–153
Demay A (1946) Sur la nappe anté-stéphanienne de la Margeride dans la région médiane du Masisf central. C R Acad Sci Paris D 222:1119–1121
Dudek A (1980) The crystalline basement block of the outher Carpathians in Moravia: Brunovistulicum. Rozpr. Cs. Akad. Ved, R. mat. prir. ved, Praha 90:1–85
Edel JB, Schulmann K, Holub FV (2003) Anticlockwise and clockwise rotations of the Eastern Variscides accommodated by dextral lithospheric wrenching: palaeomagnetic and structural evidence. J Geol Soc 160:209–218. https://doi.org/10.1144/0016-764902-035
England PC, Richardson SW (1977) The influence of erosion upon the mineral facies of rocks from different metamorphic environments. J Geol Soc 134:201–213. https://doi.org/10.1144/gsjgs.134.2.0201
England PC, Thompson AB (1984) Pressure temperature time paths of regional metamorphism. 1. Heat-transfer during the evolution of regions of thickened continental-crust. J Petrol 25:894–928
England P, Le Fort P, Molnar P, Pecher A (1992) Heat sources for tertiary metamorphism and anatexis in the Annapurna-Manaslu region central Nepal. J Geophys Res Solid Earth 97:2107–2128. https://doi.org/10.1029/91JB02272
Fediuková E, Fišera M, Cháb J, Kopečný V, Opletal M, Rybka R (1985) Garnets of the pre-Devonian rocks in the eastern part of the Hrubý Jeseník Mts. (North Moravia, Czechoslovakia). Acta Univ Carol Geol 3:197–234
Finger F, Tichomirowa M, Pin C, Hanzl P (2000) Relics of an early-Panafrican metabasite-metarhyolite formation in the Brno Massif, Moravia, Czech Republic. Int J Earth Sci 89:328–335. https://doi.org/10.1007/s005310000084
Foster G, Kinny P, Vance D, Prince C, Harris N (2000) The significance of monazite U–Th–Pb age data in metamorphic assemblages; a combined study of monazite and garnet chronometry. Earth Planet Sci Lett 181:327–340. https://doi.org/10.1016/S0012-821X(00),00212-0
Franěk J, Schulmann K, Lexa O, Tomek C, Edel JB (2011) Model of syn-convergent extrusion of orogenic lower crust in the core of the Variscan belt: implications for exhumation of high-pressure rocks in large hot orogens. J Metamorph Geol 29:53–78. https://doi.org/10.1111/j.1525-1314.2010.00903.x
Friedl G, Finger F, Paquette JL, von Quadt A, McNaughton NJ, Fletcher IR (2004) Pre-Variscan geological events in the Austrian part of the Bohemian Massif deduced from U–Pb zircon ages. Int J Earth Sci 93:802–823. https://doi.org/10.1007/s00531-004-0420-9
Fritz H (1996) Geodynamic and tectonic evolution of the southeastern Bohemian Massif: the Thaya section (Austria). Mineral Petrol 58:253–278
Fritz H, Dallmeyer RD, Neubauer F (1996) Thick-skinned versus thin-skinned thrusting: rheology controlled thrust propagation in the Variscan collisional belt (The southeastern Bohemian Massif, Czech Republic—Austria). Tectonics 15:1389–1413. https://doi.org/10.1029/96TC01098
Gasser D, Bruand E, Rubatto D, Stüwe K (2012) The behaviour of monazite from greenschist facies phyllites to anatectic gneisses: an example from the Chugach Metamorphic Complex, southern Alaska. Lithos 134–135:108–122. https://doi.org/10.1016/j.lithos.2011.12.003
Graham CM, England PC (1976) Thermal regimes and regional metamorphism in vicinity of overthrust faults—an example of shear heating and inverted metamorphic zonation from Southern-California. Earth Planet Sci Lett 31:142–152
Grujic D, Casey M, Davidson C, Hollister LS, Kündig R, Pavlis T, Schmid S (1996) Ductile extrusion of the Higher Himalayan Crystalline in Bhutan: evidence from quartz microfabrics. Tectonophysics 260:21–43
Guillot S, Allemand P (2002) Two-dimensional thermal modelling of the early tectonometamorphic evolution in Central Himalaya. J Geodyn 34:77–98. https://doi.org/10.1016/S0264-3707(02)00016-9
Hacker B, Kylander-Clark A, Holder R (2019) REE partitioning between monazite and garnet: implications for petrochronology. J Metamorph Geol 37:227–237. https://doi.org/10.1111/jmg.12458
Harrison TM, Grove M, Lovera OM, Catlos EJ (1998) A model for the origin of Himalayan anatexis and inverted metamorphism. J Geophys Res B Solid Earth 103:27017–27032
Hermann J, Rubatto D (2003) Relating zircon and monazite domains to garnet growth zones: age and duration of granulite facies metamorphism in the Val Malenco lower crust. J Metamorph Geol 21:833–852. https://doi.org/10.1046/j.1525-1314.2003.00484.x
Höck V (1975) Mineralzonen in Metapeliten und Metapsammiten der Moravischen Zone in Niederoesterreich. 66–67:49–60
Höck V, Marschallinger R, Topa D (1990) Granat-biotit-geothermometrie in metapeliten der Moravischen Zone in Osterreich. Acta Univ Carol Geol 3:149–167
Holland TJB, Powell R (1998) An internally consistent thermodynamic data set for phases of petrological interest. J Metamorph Geol 16:309–343
Holland T, Powell R (2003) Activity-compositions relations for phases in petrological calculations: an asymetric multicomponent formulation. Contrib Mineral Petrol 145:492–501. https://doi.org/10.1007/s00410-003-0464-z
Hubbard MS (1996) Ductile shear as a cause of inverted metamorphism: example from the Nepal Himalaya. 104:493–499. https://doi.org/10.1086/629842
Jamieson RA, Beaumont C, Hamilton J, Fullsack P (1996) Tectonic assembly of inverted metamorphic sequences. Geology 24:839–842. https://doi.org/10.1130/0091-7613(1996)024%3c0839:TAOIMS%3e2.3.CO;2
Jamieson RA, Beaumont C, Nguyen MH, Lee B (2002) Interaction of metamorphism, deformation and exhumation in large convergent orogens. J Metamorph Geol 20:9–24. https://doi.org/10.1046/j.0263-4929.2001.00357.x
Jiang Y, Štípská P, Sun M, Schulmann K, Zhang J, Wu Q, Long X, Yuan C, Racek M, Zhao G, Xiao W (2015) Juxtaposition of barrovian and migmatite domains in the chinese altai: a result of crustal thickening followed by doming of partially molten lower crust. J Metamorph Geol 33:45–70. https://doi.org/10.1111/jmg.12110
Johnson MRW (2005) Structural settings for the contrary metamorphic zonal sequences in the internal and external zones of the Himalaya. J Asian Earth Sci 25:695–706. https://doi.org/10.1016/j.jseaes.2004.04.010
Jung J, Roques M (1936) Les zones d'isométamorphisme dans le terrain cristallophyllien du Massif Central français. Rev Sc Nat Auvergne Tome I Fasc 4:38–85
Kidder S, Ducea MN (2006) High temperatures and inverted metamorphism in the schist of Sierra de Salinas, California. Earth Plan Sci Lett 241:422–437. https://doi.org/10.1016/j.epsl.2005.11.037
Konopásek J, Schulmann K, Johan V (2002) Eclogite-facies metamorphism at the eastern margin of the Bohemian Massif—subduction prior to continental underthrusting? Eur J Mineral 14:701–713. https://doi.org/10.1127/0935-1221/2002/0014-0701
Košler J, Konopásek J, Sláma J, Vrána S (2014) U-Pb zircon provenance of Moldanubian metasediments in the Bohemian Massif. J Geol Soc 171:83–95. https://doi.org/10.1144/jgs2013-059
Košuličová M, Štípská P (2007) Variations in the transient prograde geothermal gradient from chloritoid-staurolite equilibria: a case study from the Barrovian and Buchan-type domains in the Bohemian Massif. J Metamorph Geol 25:19–35. https://doi.org/10.1111/j.1525-1314.2006.00674.x
Kusbach V, Ulrich S, Schulmann K (2012) Ductile deformation and rheology of sub-continental mantle in a hot collisional orogeny: example from the Bohemian Massif. J Geodyn 56–57:108–123. https://doi.org/10.1016/j.jog.2011.06.004
Kusbach V, Janoušek V, Hasalová P, Schulmann K, Fanning CM, Erban V, Ulrich S (2015) Importance of crustal relamination in origin of the orogenic mantle peridotite–high-pressure granulite association: example from the Náměšť granulite massif (Bohemian Massif, Czech Republic). J Geol Soc 172:479–490. https://doi.org/10.1144/jgs2014-070
Kylander-Clark ARC (2017) Petrochronology by laser-ablation inductively coupled plasma mass spectrometry. Rev Mineral Petrol 83:183–196. https://doi.org/10.2138/rmg.2017.83.6
Kylander-Clark ARC, Hacker BR, Cottle JM (2013) Laser-ablation split-stream ICP petrochronology. Chem Geol 345:99–112. https://doi.org/10.1016/j.chemgeo.2013.02.019
Le Fort P (1975) Himalayas: the collided range, present knowledge of the continental arc. Am J Sci 275A:1–44
Ludwig KR (2003) Isoplot 3.00. A geochronological toolkit for Microsoft Excel. 4:1–70
Mahar EM, Baker JM, Powell R, Holland TJB, Howell N (1997) The effect of Mn on mineral stability in metapelites. J Metamorp Geol 15:223–238. https://doi.org/10.1111/j.1525-1314.1997.00011.x
Maierová P, Lexa O, Schulmann K, Štípská P (2014) Contrasting tectono-metamorphic evolution of orogenic lower crust in the Bohemian Massif: a numerical model. Gondwana Res 25:509–521. https://doi.org/10.1016/j.gr.2012.08.020
Molnar P, England P (1990) Temperatures, heat flux, and frictional stress near major thrust faults. J Geophys Res Solid Earth 95:4833–4856. https://doi.org/10.1029/jb095ib04p04833
Nahodilová R, Štípská P, Powell R, Košler J, Racek M (2014) High-Ti muscovite as a prograde relict in high pressure granulites with metamorphic Devonian zircon ages (Běstvina granulite body, Bohemian Massif): consequences for the relamination model of subducted crust. Gondwana Res 25:630–648. https://doi.org/10.1016/j.gr.2012.08.021
Paton C, Hellstrom J, Paul B, Woodhead J, Hergt J (2011) Iolite: freeware for the visualisation and processing of mass spectrometric data. J Anal At Spectrom 26:2508–2518. https://doi.org/10.1039/c1ja10172b
Pecher A (1989) The metamorphism in the Central Himalaya. J Metamorp Geol 7:31–41
Peřestý V, Lexa O, Holder R, Jeřábek P, Racek M, Štípská P, Schulmann K, Hacker B (2017) Metamorphic inheritance of Rheic passive margin evolution and its early-Variscan overprint in the Teplá-Barrandian Unit, Bohemian Massif. J Metamorph Geol 35:327–355. https://doi.org/10.1111/jmg.12234
Pertoldová J, Verner K, Vrána S, Buriánek D, Štědrá V, Vondrovic L (2010) Comparison of lithology and tectonometamorphic evolution of units at the northern margin of the Moldanubian Zone: implications for geodynamic evolution in the northeastern part of the Bohemian Massif. J Geosciences 55:299–319. https://doi.org/10.3190/jgeosci.083
Petri B, Štípská P, Skrzypek E, Schulmann K, Corsini M, Franěk J (2014) Thermal and mechanical behaviour of the orogenic middle crust during the syn- to late-orogenic evolution of the Variscan root zone, Bohemian Massif. J Metamorph Geol 32:599–626. https://doi.org/10.1111/jmg.12081
Pfiffner OA (2016) Basement-involved thin-skinned and thick-skinned tectonics in the Alps. Geol Mag 153:1085–1109. https://doi.org/10.1017/S0016756815001090
Pitra P, Guiraud M (1996) Probable anticlockwise P–T evolution in extending crust: hlinsko region, Bohemian Massif. J Metamorph Geol 14:49–60
Powell R, Holland T, Worley B (1998) Calculating phase diagrams involving solid solutions via non-linear equations, with examples using THERMOCALC. J Metamorph Geol 16:577–588. https://doi.org/10.1111/j.1525-1314.1998.00157.x
Preclik K (1924) Zur Analyse des Moravischen Faltenwurfes im Thayatale 180–191
Preclik K (1926) Das Nordende der Thayakuppel 6:373–399
Pyle JM, Spear FS (1999) Yttrium zoning in garnet: coupling of major and accessory phases during metamorphic reactions. Geol Mater Res 1:1–49
Pyle JM, Spear FS, Rudnick RL, McDonough WF (2001) Monazite-xenotime-garnet equilibrium in metapelites and a new monazite-garnet thermometer. J Petrol 42:2083–2107
Racek M, Štípská P, Pitra P, Schulmann K, Lexa O (2006) Metamorphic record of burial and exhumation of orogenic lower and middle crust: a new tectonothermal model for the Drosendorf window (Bohemian Massif, Austria). Mineral Petrol 86:221–251. https://doi.org/10.1007/s00710-005-0111-7
Racek M, Lexa O, Schulmann K, Corsini M, Štípská P, Maierová P (2017) Re-evaluation of polyphase kinematic and 40Ar/39Ar cooling history of Moldanubian hot nappe at the eastern margin of the Bohemian Massif. Int J Earth Sci 106:397–420. https://doi.org/10.1007/s00531-016-1410-4
Schulmann K (1990) Fabric and kinematic study of the Bíteš orthogneiss (southwestern Moravia): result of large-scale northeastward shearing parallel to the Moldanubian/Moravian boundary. Tectonophysics 177:229–244. https://doi.org/10.1016/0040-1951(90)90283-E
Schulmann K, Gayer R (2000) A model for a continental accretionary wedge developed by oblique collision: the NE Bohemian Massif. J Geol Soc 157:401–416. https://doi.org/10.1144/jgs.157.2.401
Schulmann K, Ledru P, Autran A, Melka R, Lardeaux JM, Urban M, Lobkowicz M (1991) Evolution of nappes in the eastern margin of the Bohemian Massif: a kinematic interpretation. Geol Rundsch 80:73–92. https://doi.org/10.1007/BF01828768
Schulmann K, Melka R, Lobkowicz MZ, Ledru P, Lardeaux JM, Autran A (1994) Contrasting styles of deformation during progressive nappe stacking at the southeastern margin of the Bohemian Massif (Thaya Dome). J Struct Geol 16:355–370. https://doi.org/10.1016/0191-8141(94)90040-X
Schulmann K, Lobkowicz M, Melka R, Fritz H (1995) Structure of the allochthonous Moravo-Silesian units. In: Dallmeyer RD, Franke W, Weber K (eds) Pre-Permian Geology of Central and Eastern Europe. Springer, Berlin, pp 530–540
Schulmann K, Kröner A, Hegner E, Wendt I, Konopásek J, Lexa O, Štípská P (2005) Chronological constraints on the pre-orogenic history, burial and exhumation of deep-seated rocks along the eastern margin of the Variscan orogen, Bohemian Massif, Czech Republic. Am J Sci 305:407–448. https://doi.org/10.2475/ajs.305.5.407
Schulmann K, Martelat JE, Ulrich S, Lexa O, Štípská P, Becker JK (2008) Vertical extrusion and horizontal channel flow of orogenic lower crust: key exhumation mechanisms in large hot orogens? J Metamorph Geol 26:273–297. https://doi.org/10.1111/j.1525-1314.2007.00755.x
Schulmann K, Konopásek J, Janoušek V, Lexa O, Lardeaux JM, Ede JB, Štípská P, Ulrich S (2009) An Andean type Palaeozoic convergence in the Bohemian Massif. C R Geosci 341:266–286. https://doi.org/10.1016/j.crte.2008.12.006
Schulmann K, Lexa O, Janoušek V, Lardeaux JM, Edel JB (2014) Anatomy of a diffuse cryptic suture zone: an example from the Bohemian Massif, European variscides. Geology 42:275–278. https://doi.org/10.1130/G35290.1
Searle MP, Rex AJ (1989) Thermal model for the Zanskar Himalaya. J Metamorph Geol 7:127–134. https://doi.org/10.1111/j.1525-1314.1989.tb00579.x
Soejono I, Žáčková E, Janoušek V, Machek M, Košler J (2010) Vestige of an Early Cambrian incipient oceanic crust incorporated in the Variscan orogen: letovice Complex, Bohemian Massif. J Geol Soc 167:1113–1130. https://doi.org/10.1144/0016-76492009-180
Souček J (1978) Metamorphic zones of the Vrbno and Rejvíz series, the Hrubý Jeseník Mountains. Czechoslovakia. 25:195–217
Stacey JS, Kramers JD (1975) Approximation of terrestrial lead isotope evolution by a two-stage model. Earth Plan Sci Lett 26:207–221. https://doi.org/10.1016/0012-821X(75)90088-6
Štípská P, Schulmann K (1995) Inverted metamorphic zonation in a basement-derived nappe sequence, eastern margin of the Bohemian Massif. Geol J 30:385–413. https://doi.org/10.1002/gj.3350300315
Štípská P, Schulmann K, Höck V (2000) Complex metamorphic zonation of the Thaya dome: result of buckling and gravitational collapse of an imbricated nappe sequence vol 169. https://doi.org/10.1144/gsl.sp.2000.169.01.15
Štípská P, Schulmann K, Kröner A (2004) Vertical extrusion and middle crustal spreading of omphacite granulite: a model of syn-convergent exhumation (Bohemian Massif, Czech Republic). J Metamorph Geol 22:179–198. https://doi.org/10.1111/j.1525-1314.2004.00508.x
Štípská P, Schulmann K, Powell R (2008) Contrasting metamorphic histories of lenses of high-pressure rocks and host migmatites with a flat orogenic fabric (Bohemian Massif, Czech Republic): a result of tectonic mixing within horizontal crustal flow? J Metamorph Geol 26:623–646. https://doi.org/10.1111/j.1525-1314.2008.00781.x
Štípská P, Hacker BR, Racek M, Holder R, Kylander-Clark ARC, Schulmann K, Hasalová P (2015) Monazite dating of prograde and retrograde P-T-d paths in the Barrovian terrane of the Thaya window, Bohemian Massif. J Pet 56:1007–1035. https://doi.org/10.1093/petrology/egv026
Štípská P, Powell R, Hacker BR, Holder R, Kylander-Clark ARC (2016) Uncoupled U/Pb and REE response in zircon during the transformation of eclogite to mafic and intermediate granulite (Blanský les, Bohemian Massif). J Metamorph Geol 34:551–572. https://doi.org/10.1111/jmg.12193
Suess FE (1912) Die Moravischen Fenster und ihre Beziehung zum Grundgebirge des Hohen Gesenkes. Kaiserlich-königlichen Hof-und Staatsdruckerei 88:541–631
Suess FE (1926) Intrusionstektonik und Wandertektonik im variszichen Grundgebirge. Verlag Bornttrager, Berlin
Tajčmanová L, Konopásek J, Schulmann K (2006) Thermal evolution of the orogenic lower crust during exhumation within a thickened Moldanubian root of the Variscan belt of Central Europe. J Metamorph Geol 24:119–134. https://doi.org/10.1111/j.1525-1314.2006.00629.x
Tajčmanová L, Soejono I, Konopásek J, Košler J, Klötzli U (2010) Structural position of high-pressure felsic to intermediate granulites from NE Moldanubian domain (Bohemian Massif). J Geol Soc 167:329–345. https://doi.org/10.1144/0016-76492009-086
Tollmann A (1982) Großräumiger variszischer Deckenbau im Moldanubikum und neue Gedanken zum Variszikum Europas 64:1–91
Treloar PJ, Broughton RD, Williams MP, Coward MP, Windley BF (1989) Deformation, metamorphism and imbrication of the Indian plate, south of the Main Mantle Thrust, north Pakistan. J Metamorph Geol 7:111–125. https://doi.org/10.1111/j.1525-1314.1989.tb00578.x
Ulrich S, Schulmann K, Casey M (2002) Microstructural evolution and rheological behaviour of marbles deformed at different crustal levels. J Struct Geol 24:979–995. https://doi.org/10.1016/S0191-8141(01)00132-8
White RW, Powel R, Holland TJB, Worley B (2000) The effect of TiO2 and Fe2O3 on metapelitic assemblages at greenschist and amphibolite facies conditions: mineral equilibria calculations in the system K2O–FeO–MgO–Al2O3–SiO2–H2O–TiO2–Fe2O3. J Metamorph Geol 18:497–511. https://doi.org/10.1046/j.1525-1314.2000.00269.x
White RW, Pomroy NE, Powell R (2005) An in situ metatexite-diatexite transition in upper amphibolite facies rocks from Broken Hill, Australia. J Metamorph Geol 23:579–602. https://doi.org/10.1111/j.1525-1314.2005.00597.x
White RW, Powell R, Holland TJB (2007) Progress relating to calculation of partial melting equilibria for metapelites. J Metamorph Geol 25:511–527. https://doi.org/10.1111/j.1525-1314.2007.00711.x
Wing BA, Ferry JM, Harrison TM (2003) Prograde destruction and formation of monazite and allanite during contact and regional metamorphism of pelites: petrology and geochronology. Contrib Mineral Petrol 145:228–250. https://doi.org/10.1007/s00410-003-0446-1
Acknowledgements
This work was supported by the Czech Science Foundation (grant number 19-25035S). B.R.H. acknowledges National Science Foundation grant EAR-1551054. M. K. benefited from financial support of the French embassy during her stays at the Strasbourg University, France. R. Čopjaková and R. Škoda from the Institute of Geosciences, Masaryk University, Brno are thanked for operating the microprobe during monazite mapping. We thank A. Willner and an anonymous reviewer for constructive comments and P. Hasalová for her editorial work.
Author information
Authors and Affiliations
Corresponding author
Electronic supplementary material
Below is the link to the electronic supplementary material.
Rights and permissions
About this article
Cite this article
Štípská, P., Schulmann, K., Racek, M. et al. Finite pattern of Barrovian metamorphic zones: interplay between thermal reequilibration and post-peak deformation during continental collision—insights from the Svratka dome (Bohemian Massif). Int J Earth Sci (Geol Rundsch) 109, 1161–1187 (2020). https://doi.org/10.1007/s00531-019-01788-6
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00531-019-01788-6