Experimental constraints on the formation of high-P/high-T granulites in the Southern Bohemian Massif

European Journal of Mineralogy

Volumn 17, Issue 2, 2005, Pages 343-356

  Tropper, Peter ^a   Konzett, Jürgen ^a   Finger, Friedrich ^b  

^a UNIVERSITY OF INNSBRUCK   (Austria)

^b UNIVERSITY OF SALZBURG   (Austria)

Author keywords

Bohemian Massif; Dehydration melting; High P high T granulites; Piston cylinder experiments

Indexed keywords

BIOTITE; CYLINDERS (SHAPES); GARNETS; METAMORPHIC ROCKS; MICA; PHOSPHATE MINERALS; PISTONS; QUARTZ; STRUCTURAL GEOLOGY; TITANIUM; TITANIUM DIOXIDE; ZIRCON;

ACCESSORY MINERALS; BOHEMIAN MASSIFS; CHEMICAL COMPOSITIONS; EXPERIMENTAL CONDITIONS; HIGH-P/HIGH-T GRANULITES; MINERAL COMPOSITION; PISTON CYLINDERS; VARISCAN OROGENIES;

FELDSPAR;

ACCESSORY MINERAL; GRANULITE; HERCYNIAN OROGENY; METAMORPHIC ROCK; PARAGENESIS;

BOHEMIAN MASSIF; CENTRAL EUROPE; EASTERN HEMISPHERE; EURASIA; EUROPE; WORLD;

EID: 18444393422     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2005/0017-0343     Document Type: Article

References (63)

1. Amthauer, G. & Rossman, G. (1998): The hydrous component in andradite garnet. Am. Mineral., 83, 835-840.
2. Aranovich, L. Ya. & Berman, R. G. (1996): Optimized standard state and solution properties of minerals; II, Comparisons, predictions, and applications. Contrib. Mineral. Petrol., 126, 25-37.
3. Armbruster, T., Birrer, J., Libowitzky, E., Beran, A. (1998): Crystal chemistry of Ti-bearing andradites. Eur J. Mineral., 10, 907-921.
4. Becker, H. (1997): Sm-Nd ages and cooling history of high-temperature garnet peridotite massifs and high-pressure granulites from Lower Austria. Contrib. Mineral. Petrol., 127, 224-236.
5. 2. J. Petrol., 29, 445-522.
6. 2. Contrib. Mineral. Petrol., 126 1-24.
7. Carrington, D. P. & Harley, S. L. (1995): Partial melting and phase relations in high-grade metapelites: an experimental petrogenetic grid in the KFMASH system. Contrib. Mineral. Petrol., 120, 270-291.
8. Carrington, D. P. & Watt, G. R. (1995): A geochemical and experimental study of the role of K-feldspar during water-undersaturated melting of metapelites. Chemical Geol., 122, 59-76.
9. Carswell, D. A. (1991.): Variscan high P-T metamorphism and uplift history in the Moldanubian Zone of the Bohemian Massif in Lower Austria. Eur. J. Mineral., 3, 323-342.
10. Castro, A., Patino Douce, A. E., Guillermo Corretgé, L., de la Rosa, J. D., El-Biad, M. & El-Hmidi, H. (1999): Origin of peraluminous granites and granodiorites, Iberian massif, Spain: an experimental test of granite petrogenesis. Contrib. Mineral. Petrol., 135, 255-276.
11. Clemens, J. D. (1990): The granulite-granite connection. In Vielzeuf, D. & Vidal, P. (eds.) Granulites and Crustal Evolution. Kluwer Academic Publishers, Dordrecht, Holland, 25-36.
12. Clemens, J. D. & Vielzeuf, D. (1987): Constraints on melting and magma production in the crust. Earth Planet. Sci. Lett., 86, 287-306.
13. Clemens, J. D. & Wall, V. J. (1981): Origin and crystallization of some peraluminous (S-type) granitic magmas. Can. Mineral., 19, 111-131.
14. 2 at P ≤51.5 GPa. Contrib. Mineral. Petrol. 129, 308-325.
15. Cooke, R. A. (2000): High pressure/temperature metamorphism in the St.Leonhard Granulite Massif, Austria: evidence from intermediate pyroxene-bearing granulites. Int. J. Earth Sciences, 89, 631-651.
16. Cooke, R. A. & O'Brien, P. J. (2001): Resolving the relationship between high P-T rocks and gneisses in collisional terranes: an example from the Gföhl gneiss-granulite association in the Moldanubian Zone, Austria. Lithos, 58, 33-54.
17. Donohue, C. L., Manning, C. E., Essene, E. J. (2001): The pressure and temperature dependence of Zr and Ti substitution in almandine. Geol. Soc. Amer. Abstr., 33, 251.
18. Dudek, A., Matejovska, O., Suk, M. (1974): Gföhl orthogneiss in the Moldanubicum of Bohemia and Moravia. Krystalinikum, 10, 67-78.
19. Elkins, L. T. & Grove, T. L. (1990): Ternary feldspar experiments and thermodynamic models. Am. Mineral., 75, 544-559.
20. Fiala, J., Matejovska, O., Vankova, V. (1987): Moldanubian granulites: source material and petrogenetic considerations. N. Jb. Mineral. Abh. 157, 133-165.
21. Finger, F., Roberts, M. P., Pöschl-Otrel, K., Haunschmid, B. (1996): Anzeichen für partielle Anatexis und späte Zirkonkristallisation in moldanubischen Hochdruck-Granuliten aus Niederösterreich. Terra Nostra, 96/2, 48-51.
22. Franke, W. (1989): Tectonostratigraphic units in the Variscan belt of Central Europe. Geol. Soc. Am. Spec. Paper, 230, 67-90.
23. Fuhrman, L. & Lindsley, D. H. (1988): Ternary-feldspar modelling and thermometry. Am. Mineral., 73, 201-215.
24. Gardien, V., Thompson, A. B., Grujic, D., Ulmer, P. (1995): Experimental melting of biotite + plagioclase + quartz ± muscovite assemblages for crustal melting. J. Geophys. Res., 100, 15581-15591.
25. Grant, J. A. (1985): Phase equilibria in partial melting of pelitic rocks. In Ashowrth, J. R. (ed.) Migmatites. Blackie, Glasgow, 86-144.
26. Harley, S. L. (1989): The origins of granulites: a metamorphic perspective. Geol. Mag., 126, 215-247.
27. Holland, T. J. B. & Powell, R. (1998): An internally-consistent thermodynamic data set for phases of petrological interest. J. metamorphic Geol., 8, 89-124.
28. 2O-activities. J. Petrol., 32, 935-957.
29. 2O on liquidus phase relations in the haplogranite system at 2 and 5 kbar. Am. Mineral., 77, 1223-1241.
30. Holtz, F., Johannes, W., Tamic, N., Behrens, H. (2001): Maximum and minimum water contents of granitic melts generated in the crsust: a re-evaluation and implications. Lithos, 56, 1-14.
31. Jakes, P. (1997): Melting in high-P region - case of Bohemian granulites. Acta Univ. Carol., Geol., 41, 113-125.
32. Janousek, V., Finger, F., Roberts, M., Fryda, J., Pin, C., Dolejs, D. (2005): Deciphering petrogenesis of deeply buried granites: whole-rock geochemical constraints on the origin of largely undepleted felsic granulites from the Moldanubian Zone of the Bohemian Massif. Trans. Royal Soc. Edinburgh, 95, 141-159.
33. Johannes, W. & Holtz, F. (1996): Petrogenesis and Experimental Petrology of Granitic Rocks. Springer Verlag, Berlin, 335 p.
34. Keane, S. D., Essene, E. J., Manning, C. E. (1997): Trace-element thermobarometry using titanium in garnet. Seventh annual V. M. Goldschmidt Conf., LPI Contribution, 921, 110-111.
35. Kotková, J. & Harley, S. L. (1999): Formation and evolution of high-pressure leucogranulites; experimental constraints and unresolved issues. In Brown, M. G. & Kotková, J. (eds.) Crust melting in nature and experiment. Phys. Chem. Earth Part A: Solid Earth and Geodesy, 24, 299-304.
36. Kretz, R. (1983): Symbols for rock-forming minerals. Am. Mineral., 68, 277-279
37. Le Breton, N. & Thompson, A. B. (1988): Fluid-absent (dehydration) melting of biotite in metapelites in the early stages of crustal anatexis. Contrib. Mineral. Petrol., 99, 226-237.
38. Linner, M. (1996): Metamorphism and partial melting of paragneisses of the Monotonous Group, SE Moldanubicurn (Austria). Mineral. Petrol. 58, 215-234.
39. Litvinovsky, B. A., Steele, I. M., Wickham, S. M. (2000): Silicic magma formation in overthickened crust: melting of charnockite and leucogranite at 15, 20 and 25 kbar. J. Petrol., 41, 717-737.
40. Montel, J. M. & Vielzeuf, D. (1996): Partial melting of metagrey-wackes. II. Compositions of minerals and melts. Contrib. Mineral. Petrol., 128, 176-196.
41. Müntener, O. & Hermann, J. (1994): Titanian andradite in a metapyroxenite layer from the Malenco ultramafics (Italy): implications for Ti-mobility and low oxygen fugacity. Contrib. Mineral. Petrol. 116, 156-168.
42. Nair, R. & Chacko, T. (2002): Fluid-absent melting of high-grade semipelites: P-T constraints on orthopyroxene formation and implications for granulite genesis. J. Petrol., 43, 2121-2142.
43. O'Brien, P. J. (1999): Asymmetric zoning profiles in garnet from HP-HT granulite and implications for volume and grain boundary diffusion. Mineral. Mag., 63, 227-238.
44. O'Brien, P. J. & Carswell, D. A. (1993): Tectonometamorphic evolution of the Bohemian Massif: evidence from high-P metamorphic rocks. Geol. Rundsch., 82: 531-555.
45. O'Brien, P. J. & Rötzler, J. (2003): High-pressure granulites: formation, recovery of peak conditions and implications for tectonics. J. metamorphic Geol., 21, 3-20.
46. Patino-Douce, A. E. & Beard, J. S. (1995): Dehydration melting of biotite gneiss and quartz amphibolite from 3 to 15 kbar. J. Petrol. 36, 707-738.
47. 2) and Mg/Fe ratio on dehydration melting of model metagreywackes. J. Petrol., 37, 999-1024.
48. Patino-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. Contrib. Mineral. Petrol., 107, 202-218.
49. Petrakakis, K. (1997): Evolution of Moldanubian rocks in Austria: a review and synthesis. J. metamorphic Geol., 15, 203-222.
50. Roberts, M. P. & Finger, F. (1997): Do U-Pb zircon ages from granulites reflect peak metamorphic conditions? Geology, 25, 319-322.
51. Scharbert, H. G. (1971): Granulitfazien im Moldanubikum der Böhmischen Masse Niederösterreichs. Freiberger Forschungsh., 268, 81-89.
52. Scharbert, H. G. & Kurat, G. (1974): Distribution of some elements between coexisting ferromagnesioan minerals in Moldanubian granulite facies rocks, Lower Austria, Austria. Tschermaks Min. Petrolog. Mitt. 21, 110-134.
53. Skjerlie, K. P. & Johnston, A. D. (1996): Vapour-absent melting from 10 to 20 kbar of crustal rocks that contain multiple hydrous phases: implications for anatexis in the deep to very deep continental crust and active continental margins. J. Petrol., 37, 661-691.
54. Stevens, G. & Clemens, J. D. (1993): Fluid-absent melting and the roles of fluids in the lithosphere: a slanted summary? Chemical Geol., 108, 1-17.
55. Stevens, G., Clemens, J. D., Droop, G. (1997): Melt production during granulite-facies anatexis: experimental data from "primitive" metasedimentary protoliths. Contrib. Mineral. Petrol., 128, 352-370.
56. 2O-understurated granitic liquids. Am. J. Sci., 282, 1567-1595.
57. Truckenbrodt, J., Ziegenbein, D., Johannes, W. (1997): Redox conditions in piston-cylinder apparatus; the different behavior of boron nitride and unfired pyrophyllite assemblies. Am. Mineral., 82, 337-344.
58. Vielzeuf, D. & Holloway, J. R. (1988): Experimental determination of the fluid-absent melting relations in the pelitic system: consequences for crustal differentiation. Contrib. Mineral. Petrol., 98, 257-276.
59. Vielzeuf, D. & Montel, J. M. (1994): Partial melting of metagreywackes. I. Fluid-absent experiments and phase relationships. Contrib. Mineral. Petrol., 117, 375-393.
60. Vielzeuf, D. & Schmidt, M. W. (2001): Melting relations in hydrous systems revisited: application to metapelites, metagreywackes and metabasalts. Contrib. Mineral. Petrol., 141, 251-267.
61. Vrana, S. (1989): Perpotassic granulites from southern Bohemia: a new rock-type derived from partial melting of crustal rocks under upper mantle conditions. Contrib. Mineral. Petrol., 103, 510-522.
62. Winkler, H. G. F. & von Platen, H. (1961): Experimentelle Gesteinsmetamorphose. Geochim. Cosmochim. Acta, 24, 250-259.
63. 2 pressures. Unpubl. Ph.D. Thesis, University of Chicago, 266 pp.