High-temperature to ultrahigh-temperature metamorphism related to multiple ultrapotassic intrusions: Evidence from garnet-sillimanite-cordierite kinzigite and garnet-orthopyroxene migmatites in the eastern part of the Moldanubian Zone (Bohemian Massif)

Geologica Carpathica

Volumn 58, Issue 5, 2007, Pages 415-425

  Leichmann, Jaromír ^a   Novák, Milan ^a   Buriánek, David ^b   Burger, David ^a  

^a MASARYK UNIVERSITY   (Czech Republic)

^b CZECH GEOLOGICAL SURVEY   (Czech Republic)

Author keywords

Garnet sillimanite rock; Heat source; HT metamorphism; Jihlava Pluton; Mineral reactions; Moldanubian Zone; Restite

Indexed keywords

CHEMICAL COMPOSITION; CORDIERITE; GARNET; HEAT SOURCE; MIGMATITE; ORTHOPYROXENE; P-T CONDITIONS; PLUTON; POTASSIC ROCK; RESTITE; SILLIMANITE; ULTRAHIGH TEMPERATURE METAMORPHISM;

BOHEMIAN MASSIF; CENTRAL EUROPE; EURASIA; EUROPE;

EID: 36549071595     PISSN: 13350552     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Article

References (40)

1. Buttner S. & Kruhl J.H. 1997: The evolution of a late-Variscan high-T/low-P region: the southeastern margin of the Bohemian massif. Geol. Rdsch. 86, 22-38.
2. Carrington D.P. & Harley S.L. 1995: Partial melting and phase relations in high-grade metapelites: an experimental petrogenetic grid in KFMASH system. Contr. Mineral. Petrology 120, 270-291.
3. Dallmeyer R.D., Franke W. & Weber K. (Eds.) 1995: Pre-Permian geology of the Central and Eastern Europe. Springer, Berlin, 1-213.
4. 3. J. Petrology 36, 435-461.
5. Deibl I., Tropper P. & Mirwald P.W. 2003: The petrological evolution of high-grade metapelites from the Sauwald, southern Bohemian Massif. Mitt. Österr. Miner. Gesell. 148, 116-117.
6. Fiala F. & Losert J. 1976: Discovery of corundum, cordierite, garnet, sillimanite and tourmaline in herynite-rich rock at Chlum near Sepekov. Čas. Mineral. Geol. 21, 326 (in Czech).
7. Franke W. 2000: The mid-European segment of the Variscides: tectonostratigraphic units, terrane boundaries and plate tectonic evolution. In: Franke W., Haak V., Oucken O. & Tanner D. (Eds.): Orogenic processes: quantification and modelling in the Variscan Belt. Geol. Soc. London, Spec. Publ. 179, 35-61.
8. Henk A., von Blanckenburg F., Finger F., Schaltegger U. & Zulauf G. 2000: Syn-convergent high-temperature metamorphism and magmatism in the Variscides: a discussion of potential heat sources. In: Franke W., Haak V., Oncken O. & Tanner D. (Eds.): Orogenic processes: quantification and modelling in the Variscan Belt. Geol. Soc. London, Spec. Publ. 179, 387-400.
9. Holtz F. & Johannes W. 1996: Petrogenesis and experimental petrology of granitic rocks. Springer, Berlin, 1-333.
10. Kalt A., Berger A. & Blümel P. 1999: Metamorphic evolution of cordierite-bearing migmatites from the Bayerische Wald (Variscan Belt, Germany). J. Petrology 40, 601-627.
11. Kotková J., Schaltegger U. & Leichmann J. 2003: 338-335 Ma old intrusion in the E Bohemian massif - a relic of the orogen-wide durbachitic magmatism in European Variscides. J. Czech. Geol. Soc. 48, 1-2, 80-81.
12. Kretz R. 1983: Symbols for rock-forming minerals. Amer. Mineralogy 68, 277-279.
13. Kriegsman L.M. & Hensen B.J. 1998: Back reaction between restite and melt: Implications for geothermobarometry and pressure-temperature paths. Geology 26, 1111-1114.
14. Leichmann J. & Švancara J. 2005: Shoshonitic to ultrapotassic gabbros from the Jihlava pluton. 2. meeting of the Czech Geol. Soc., Slavonice, 151-153 (in Czech).
15. Leichmann J., Novák M., Zachovalová K. & Topa. D. 2000: Ultra-high temperature event in the Moldanubian Zone; its significance for the origin of durbachites. Geolines 10, 47.
16. Linner M. 1996: Metamorphism and partial melting of paragneisses of the Monotonous Group, SE Moldanubicum (Austria). Mineral. Petrology 58, 215-234.
17. Montel J.M., Marignac C., Barbey P. & Pichavant M. 1992: Thermobarometry and granite genesis: Hercynian low-P, high-T Velay anatectic dome (French Massif Central). J. Metamorphic Geology 10, 1-15.
18. Nekvasil H. 1992: Feldspar crystallization in felsic magmas: a review. Trans. Roy. Soc. Edinburgh, Earth Sci. 83, 399-407.
19. Nichols G.T., Berry R.F. & Green D.H. 1992: Internally consistent gahnitic spinel-cordierite-garnet equilibria in the FMASHZn system: geothermobarometry and applications. Contr. Mineral. Petrology 111, 362-377.
20. Novák M. & Houzar S. 1996: The HT/LP metamorphism of dolomite marbles in the eastern part of the Moldanubicum; a manifestation of heat flow related to the Třebíč Durbachite Massif J. Czech. Geol. Soc. 41, 139-146.
21. O'Brien P.J. 2000: The fundamental Variscan problem: high-temperature metamorphism in different depths and high-pressure metamorphism at different temperatures. In: Franke W., Haak V., Oncken O. & Tanner D. (Eds.): Orogenic, processes: quantification and modelling in the Variscan Belt. Geol. Soc. London, Spec. Publ. 179, 369-386.
22. Patiño Douce A.E. & Johnston A.D. 1991: Phase equilibria and melt productivity in the pelitic system: implications for the origin of peraluminous granitoids and aluminous granulites. Contr. Mineral. Petrology 107, 202-218.
23. Patiño Douce A.E. & McCarthy T.C. 1998: Melting of crustal rocks during continental collision and subduction. In: Hacker B.R. & Lion J.G. (Eds.): When continents collide: geodynamics and geochemistry of ultrahigh-pressure rocks. Kluwer Academic Publishers, 27-55.
24. Petrakakis K. 1997: Evolution of Moldanubian rocks in Austria: review and synthesis. J. Metamorphic Geology 15, 203-222.
25. Pouchou J.L. & Pichoir F. 1985: "PAP" procedure for improved quantitative microanalysis. Microbeam. Anal. 20, 104-105.
26. Pownceby M.L., Wall V.J. & O'Neill H.St.C. 1991: An experimental study of effect of Ca upon garnet-ilmenite Fe-Mn exchange equilibria. Amer. Mineralogist 76, 1580-1588.
27. Sack R.O. & Ghiorso M.S. 1991: An internally consistent model for the thermodynamic properties of Fe-Mg-titano-magnetite-aluminate spinels. Contr. Mineral. Petrology 106, 474-505.
28. Sengupta P., Se J., Dasgupta S., Raith M., Bhui U.K. & Ehl J. 1999: Ultra-bigh temperature metamorphism of metapelitic granulites from Khondapalle, Eastern Ghats belt: Implications for the Indo-Antarctic correlation. J. Petrology 40, 1065-1087.
29. Shelley D. 1993: Igneous and metamorphic rocks under the microscope. Chapman & Hall, London, 1-445.
30. Shulters J.C. & Bohlen S.R. 1989: The stability of hercynite and hercynite-gahnite spinels in corundum- or quartz-bearing assemblages. J. Petrology 30, 1017-1031.
31. Spear F.S. 1993: Metamorphic, phase equilibria and pressure-temperature-time paths. Miner. Soc. Amer. Monograph, Washington, 1-799.
32. Spear F.S., Kohn M.J. & Cheney J.T. 1999: P-T paths from anatectic pelites. Contr. Mineral. Petrology 134, 17-32.
33. Thompson A.B. 1999: Some time-space relationships for crustal melting and granitic intrusions at various depths. In: Castro A., Fernandez C. & Vigneresse L. (Eds.): Understanding granites: Integrating new and classical techniques. Geol. Soc. London, Spec. Publ. 168, 7-25.
34. Tonika J. 1970: Geology and petrology of the Jihlava massif. Sbor. Geol. Věd, Ř G. 17, 105-119 (in Czech).
35. Verner K., Žák J., Holub F.V., Týcová P. & Nahodilová R. 2005: Textures and fabric of the durbachite plutons as an indicator of the tectonometamorphic evolution of the Moldanubicum (Czech Republic). 2. meeting of the Czech Geol. Soc., Slavonice, 101 (in Czech).
36. Vielzeuf D. & Holloway J.R. 1988: Experimental determination of the fluid-absent melting relations in the pelitic system: Consequences for crustal differentiation. Contr. Mineral. Petrology 98, 257-276.
37. Vielzeuf D. & Montel J.M. 1994: Partial melting of Almetagreywackes. Part I. Fluid-absent experiments and phase relationships. Contr. Mineral. Petrology 117, 375-393.
38. Waters D.J. 1991: Hercynite-quartz; granulite phase relations and implication for crustal processes. Eur. J. Mineral. 3, 567-586.
39. White R.W. & Powell R. 2002: Melt loss and the preservation of granulite facies mineral assemblages. J. Metamorphic Geology 20, 621-632.
40. Zack T., Moraes R. & Kronz A. 2004: Empirical calibration of a rutile thermometer and its application to UHT granulites. International workshop on petrogenesis of granulites and related rocks. Moravian Museum, Brno, 1-71.