The pressure-temperature path and the origin of phlogopite in spinel-garnet peridotites from the Blanský les Massif of the Moldanubian Zone, Czech Republic

Journal of Petrology

Volumn 50, Issue 10, 2009, Pages 1795-1827

  Naemura, Kosuke ^a   Hirajima, Takao ^a   Svojtka, Martin ^b  

^a KYOTO UNIVERSITY   (Japan)

^b INSTITUTE OF GEOLOGY   (Czech Republic)

Author keywords

Garnet; Metasomatism; P T conditions; Peridotite; Phlogopite

Indexed keywords

GARNET; METASOMATISM; P-T CONDITIONS; P-T-T PATH; PERIDOTITE; PHLOGOPITE;

BOHEMIAN MASSIF; CENTRAL EUROPE; EURASIA; EUROPE;

EID: 70349962938     PISSN: 00223530     EISSN: 14602415     Source Type: Journal    
DOI: 10.1093/petrology/egp052     Document Type: Article

References (94)

1. Arai, S. (1984). Pressure-temperature dependent compositional variation of phlogopitic micas in upper mantle peridotites. Contributions to Mineralogy and Petrology 87, 260-264.
2. Becker, H. (1997). Petrological constraints on the cooling history of high-temperature garnet peridotite massifs in lower Austria. Contributions to Mineralogy and Petrology 128, 272-286.
3. Becker, H. & Altherr, R. (1992). Evidence from ultrahigh pressure marbles for recycling of sediments into the mantle. Nature 358 745-748.
4. Becker, H., Wenzel, T. & Volker, F. (1999). Geochemistry of glimmerites veins in peridotites from Lower Austria - implications for the origin of K-rich magmas in collision zones. Journal of Petrology 40, 315-338.
5. Biino, C. G. & Compagnoni, R. (1992). Very-high pressure metamorphism of the Brossasco coronite metagranite, southern Dora Maira Massif, Western Alps. Schweizerische Mineralogische und Petrographische Mitteilungen 72, 347-363.
6. Boudreau, A. E., Mathez, E. A. & McCallum, I. S. (1986). Halogen geochemistry of the Stillwater and Bushveld complexes: Evidence for transport of the platinum-group elements by Cl-rich fluids. Journal of Petrology 27, 967-986.
7. Brey, G. P. & Ko
8. Brueckner, H. K. (1998). Sinking intrusion model for the emplacement of garnet-bearing peridotites into continent collision orogens. Geology 26, 631-634.
9. Brueckner, H. K. & Medaris, L. G. (2000). A general model for the intrusion and evolution of 'mantle' garnet peridotites in high-pressure and ultra-high-pressure metamorphic terranes. Journal of Metamorphic Geology 18, 123-133.
10. Bundy, F. R. (1980). The P,T phase and reaction diagram for elemental carbon, 1979. Journal of Geophysical Research 85, 6930-6938.
11. Canil, D. & O'Neill, H. St. C. (1996). Distribution of ferric ion in some upper-mantle assemblages. Journal of Petrology 37, 609-635.
12. Carswell, D. A. (1991). Variscan high P-T metamorphism and uplift history in the Moldanubian zone of the Bohemian Massif in Lower Austria. European Journal of Mineralogy 3, 323-342.
13. Carswell, D. A. & Cuthbert, S. J. (2003). Ultra-high pressure metamorphism in theWestern gneiss region of Norway. In: Carswell, D. A. & Compagnoni, R. (eds) Ultrahigh Pressure Metamorphism. EMU Notes in Mineralogy 5, 51-74.
14. Carswell, D. A. & O'Brien, P. (1993). Thermobarometry and geotectonic significance of high-pressure granulites: Examples from the Moldanubian zone of the Bohemian Massif in the Lower Austria. Journal of Petrology 34, 427-459.
15. Carswell, D. A. & Van Roermund, H. L. M. (2005). On multi-phase mineral inclusions associated with microdiamond formation in mantle-derived peridotite lens at Bardane on Fjørtoft, west Norway. EuropeanJournal of Mineralogy 17, 31-42.
16. Cooke, R. A. (2000). High-pressure/temperature metamorphism in the St. Leonhard granulite massif, Austria: Evidence from intermediate pyroxene-bearing granulites. International Journal of Earth Sciences 89, 631-651.
17. Delaney, J. S., Smith, J. V., Carswell, D. A. & Dawson, J. B. (1980). Chemistry of micas from kimberlites and xenoliths - II. Primary-and secondary-textured micas from peridotite xenoliths. Geochimica et Cosmochimica Acta 44, 857-872.
18. Exley, R. A., Sills, J. D. & Smith, J.V. (1982). Geochemistry of Micas from the Finero Spinel-Lherzolite, Italian Alps. Contributions to Mineralogy and Petrology 81, 59-63.
19. Faryad, S.W. (2009). The Kutná Hora complex (Moldanubian zone, Bohemian Massif): A composite of crustal and mantle rocks subducted to HP/UHP conditions. Lithos 109, 193-208.
20. Ferraris, C. & Compagnoni, R. (2003). Metamorphic evolution and significance of a serpentinized peridotite slice within the eclogitic micaschist complex of the Sesia-zone (Western Alps - Italy). Schweizerische Mineralogische und Petrographische Mitteilungen 83 3-13.
21. Ferrando, S., Frezzotti, M. L., Dallai, L. & Compagnoni, R. (2005). Multiphase solid inclusions in UHP rocks (Su-Lu, China): Remnants of supercritical silicate-rich aqueous fluids released during continental subduction. Chemical Geology 223, 68-81.
22. Fiala, J., Matějovská, O. & Vaňková, V. (1987). Moldanubian granulites: Source material and petrogenetic considerations. Neues Jahrbuch für Mineralogie, Abhandlungen 157, 133-165.
23. Franěk, J., Schulmann, K. & Lexa, O. (2006). Kinematic and rheological model of exhumation of high pressure granulites in the Variscan orogenic root; example of the Blanský les granulite, Bohemian Massif, Czech Republic. Mineralogy and Petrology 86 253-276.
24. Fuchs, G. (1986). Zur Diskussion um den Deckenbau der Böhmischen Masse. Jahrbuch der Geologischen Bundesanstalt 129, 41-49.
25. Fumagalli, P. & Poli, S. (2005). Experimentally determined phase relations in hydrous peridotites to 6.5 GPa and their consequences on the dynamics of subduction zones. Journal of Petrology 46, 555-578.
26. Godard, G. & Martin, S. (2000). Petrogenesis of kelyphites in garnet peridotites: A case study from the Ulten zone, Italian Alps. Journal of Geodynamics 30, 117-145.
27. Green, D. H. (1973). Experimental melting studies on a model upper mantle composition at high pressure under water-saturated and water-undersaturated conditions. Earth and Planetary Science Letters 19, 37-53.
28. Green, D. H. & Ringwood, A. E. (1967). The stability of aluminous pyroxene peridotite and garnet peridotite and their relevance in upper mantle structure. Earth and Planetary Science Letters 3, 151-160.
29. Harley, S. L. (1984). An experimental study of the partitioning of Fe and Mg between garnet and orthopyroxene. Contributions to Mineralogy and Petrology 86, 359-373.
30. Hermann, J. (2003). Experimental evidence for diamond-facies metamorphism in the Dora-Maira massif. Lithos 70, 163-182.
31. Hirajima,T. & Banno, S. (1991). Electron-Microprobe analysis of rock-forming minerals with Kevex-Delta IV Quantum Detector. Hitachi Scientific Instrument News 34, 2-7 (in Japanese).
32. Hirajima, T. & Nakamura, D. (2003). Review of representative UHPM terranes: The Dabie Shan-Sulu orogen. In: Carswell, D. A. & Compagnoni, R. (eds) Ultrahigh Pressure Metamorphism. EMU Notes in Mineralogy 5, 105-144.
33. Ionov, D. A. & Hofmann, A. W. (1995). Nb-Ta-rich mantle amphiboles and micas: Implications for subduction-related metasomatic trace element fractionations. Earth and Planetary Science Letters 131, 341-356.
34. Ionov, D. A., Ashchepkov, I. V., Stosch, H. G., Witt-Eickschen, G. & Seck, H. A. (1993). Garnet peridotite xenoliths from the Vitim Volcanic Field, Baikal Region: The nature of the garnet-spinel peridotite transition zone in the continental mantle. Journal of Petrology 34, 1141-1175.
35. Jakeš, P. (1997). Melting in high-P region - a case of Bohemian granulites. Acta Universitatis Carolinae, Geologica 41, 113-125.
36. Janoušek, V., Krenn, E., Finger, F., Míková, J. & Frýda, J. (2007). Hyperpotassic granulites from Blanský les (Moldanubian Zone, Bohemian Massif) revisited. Journal of Geosciences 52, 73-112.
37. 2. Contributions to Mineralogy and Petrology 77, 166-176.
38. Kalt, A. & Altherr, R. (1996). Metamorphic evolution of garnet-spinel peridotites from the Variscan Schwartzwald (Germany). International Journal of Earth Sciences (Geologische Rundschau) 91, 373-385.
39. Kalt, A., Altherr, R. & Hanel, M. (1995). Contrasting P-T conditions recorded in ultramafic high-pressure rocks from the Variscan Schwarzwald (F.R.G.). Contributions to Mineralogy and Petrology 121, 45-60.
40. 2 Raman spectrum indicating the transformation from coesite to quartz in Gfohl migmatitic gneisses in the Moldanubian Zone, Czech Republic. Journal of Mineralogical and Petrological Sciences 103, 105-111.
41. Kotková, J. & Harley, S. L. (1999). Formation and evolution of high-pressure leucocratic granulites: Experimental constraints and unresolved issues. Physics and Chemistry of the Earth 24, 299-304.
42. Kotková, J., Harley, S. L. & Fišera, M. (1997). A vestige of very high-pressure (ca. 28 kbar) metamorphism in the Variscan Bohemian massif, Czech Republic. European Journal of Mineralogy 9, 1017-1033.
43. 2+-Mg geothermometer: An updated calibration. Journal of Metamorphic Geology 18, 211-219.
44. Kröner, A., O'Brien, P. J., Nemchin, A. A. & Pidgeon, R. T. (2000). Zircon ages for high pressure granulites from south Bohemia, Czech Republic, and their connection to Carboniferous high temperature processes. Contributions toMineralogy and Petrology 138, 127-142.
45. Malaspina, N., Hermann, J., Scambelluri, M. & Compagnoni, R. (2006). Polyphase inclusions in garnet-orthopyroxenite (Dabie Schan, China) as monitors for metasomatism and fluid-related trace element transfer in subduction zone peridotite. Earth and Planetary Science Letters 249, 173-187.
46. Marocchi, M., Hermann, J. & Morten, L. (2007). Evidence for multi-stage metasomatism of chlorite-amphibole peridotites (Ulten zone, Italy): constraints from trace element compositions of hydrous phases. Lithos 99, 85-104.
47. Marocchi, M., Mair, V., Tropper, P. & Bargossi, G. M. (2009). Metasomatic reaction bands at the Mt. Hochwart gneiss-peridotite contact (Ulten Zone, Italy): Insight into fluid-rock interaction in subduction zones. Mineralogy and Petrology 95, 251-272.
48. Matte, P., Maluski, H., Rajlich, P. & Franke,W. (1990).Terrane boundaries in the Bohemian Massif: Result of the large-scale Variscan shearing. Tectonophysics 364, 215-235.
49. 3 II. Calibration of a combined ordering model and mixing model. Physics and Chemistry of Minerals 20, 42-55.
50. Medaris, L. G., Jr & Wang, H. H. (1986). A thermal-tectonic model for high-pressure rocks in the Basal Gneiss Complex of western Norway. Lithos 19, 299-315.
51. Medaris, L. G., Jr, Wang, H. H., Misar, Z. & Jelinek, E. (1990). Thermobarometry, diffusion modeling and cooling rates of crustal garnet peridotites: Two examples from the Moldanubian zone of the Bohemian massif. Lithos 25, 189-202.
52. Medaris, L.G., Jr,Wang, H. H., Jelinek, E., Mihaljevic,M. & Jakes, P. (2005). Characteristics and origins of diverse Variscan peridotites in the Gföhl Nappe, Bohemian massif, Czech Republic. Lithos 82 1-23.
53. Mori, T. & Kanehira, K. (1984). X-ray energy spectrometry for electron-probe analysis. Journal of Geological Society of Japan 90, 49-52.
54. Morishita,T., Arai, S. & Tamura, A. (2003). Petrology of an apatite-rich layer in the Finero phlogopite-peridotite, ItalianWestern Alps; implications for evolution of a metasomatising agent. Lithos 69 37-49.
55. Mørk, M. B. E. (1985). A gabbro to eclogite transition of Flemsoy, Summore, western Norway. In: Smith, D. C., Franz, G. & Gebauer, D. (eds) Chemistry and Petrology of Eclogites. Chemical Geology 50, 283-310.
56. Naemura, K., Yokoyama, K., Hirajima, T. & Svojtka, M. (2008). Age determination of thorianite in phlogopite-bearing spinel-garnet peridotite in the Gföhl Unit, Moldanubian zone of the Bohemian Massif. Journal of Mineralogical and Petrological Sciences 103 285-290.
57. Nazzareni, S., Braga, R., Comodi, P., Morten, L., Cera, F. & Fumagalli, P. (2005). Amphibole-Phlogopite-bearing peridotites from the Ulten Zone (Eastern Alps, Italy). Geophysical Research Abstracts 7, 08982.
58. 3): The Cr-geobarometer. In: Ross, J. (ed.) Kimberlite and Related Rocks. Geological Society of Australia, Special Publications 14, 901-912.
59. Nickel, K. G. & Green, D. H. (1985). Empirical geothermometry for garnet peridotites and implications for the nature of the lithosphere, kimberlites and diamonds. Earth and Planetary Science Letters 73, 158-170.
60. Niida, K. & Green, D. H. (1999). Stability and chemical composition of pargasitic amphibole in MORB pyrolite under upper mantle conditions. Contributions to Mineralogy and Petrology 135, 18-40.
61. Nimis, P. & Morten, L. (2000). P-T evolution of 'crustal' garnet peridotites and included pyroxenites from Nonsberg area (upper Austroalpine), NE Italy: From the wedge to the slab. Journal of Geodynamics 30, 93-115.
62. Nimis, P. & Taylor,W. R. (2000). Single clinopyroxene thermobarometry for garnet peridotites Part I. Calibration and testing of a Cr-in-Cpx barometer and an enstatite-in-Cpx thermometer. Contributions to Mineralogy and Petrology 139, 541-554.
63. Nimis, P. & Trommsdorff, V. (2001a). Revised thermobarometry of Alpe Arami and other garnet peridotites from the Central Alps. Journal of Petrology 42, 103-115.
64. Nimis, P. & Trommsdorff,V. (2001b). Comment on 'New constraints on the P-T evolution of the Alpe Arami garnet peridotite body (Central Alps, Switzerland)' by Paquin & Altherr (2001). Journal of Petrology 42, 1773-1779.
65. Obata, M. & Morten, L. (1987). Transformation of spinel lherzolite to garnet lherzolite in ultramafic lenses of the Austridic crystalline complex, northern Italy. Journal of Petrology 28, 599-623.
66. O'Neill, H. St. C. (1981). The transition between spinel lherzolite and garnet lherzolite, and its use as a geobarometer. Contributions to Mineralogy and Petrology 77, 185-194.
67. O'Neill, H. St. C. & Wood, B. J. (1979). An experimental study of Fe-Mg partitioning between garnet and olivine and its calibration as a geothermometer. Contributions toMineralogy and Petrology 70, 59-70.
68. O'Reilly, S.Y. & Griffin,W. L. (2000). Apatite in the mantle: implications for metasomatic processes and high heat production in Phanerozoic mantle. Lithos 53, 217-232.
69. Ozawa, K. (1983). Evaluation of olivine-spinel geothermometry as an indicator of thermal history for peridotites. Contributions to Mineralogy and Petrology 82, 52-65.
70. Palmeri, R., Ghiribelli, B., Ranalli, G., Talarico, F. & Ricci, C. A. (2007). Ultrahigh-pressure metamorphism and exhumation of garnet-bearing ultramafic rocks from the Lanterman Range (Northern Victorian Land, Antarctica). Journal of Metamorphic Geology 25, 225-243.
71. Paquin, J. & Altherr, R. (2001). New constraints on the P-T evolution of the Alpe Arami garnet peridotite body (central Alps, Switzerland). Journal of Petrology 42, 1119-1140.
72. Press, S.,Witt, G., Seck, H. A., Eonov, D. & Kovalenko, V. I. (1986). Spinel peridotite xenoliths from the Tariat Depression, Mongolia. I: Major element chemistry and mineralogy of a primitive mantle xenolith suite. Geochimica et Cosmochimica Acta 50, 2587-2599.
73. Rampone, E. & Morten, L. (2001). Records of crustal metasomatism in the garnet peridotites of the Ulten zone (Upper Austroalpine, Eastern Alps). Journal of Petrology 42, 207-219.
74. Ringwood, A. E., MacGregor, I. D. & Boyd, F. R. (1964). Petrological constitution of the upper mantle. Carnegie Institution Washington Yearbook 63, 147.
75. Sachtleben,Th. & Seck, H. A. (1981). Chemical control of Al-solubility in orthopyroxene and its implications on pyroxene geothermometry. Contributions to Mineralogy and Petrology 78, 157-165.
76. Scambelluri, M., Hermann, J., Morten, L. & Rampone, E. (2006). Melt- versus fluid-induced metasomatism in spinel to garnet wedge peridotites (Ulten Zone, Eastern Italian Alps): Clues from trace element and Li abundances. Contributions to Mineralogy and Petrology 151, 372-394.
77. Schmädicke, E. & Okrusch, M. (1997). Phase relations of calcic amphibole-orthoamphibole-chlorite-talc assemblages, with applications to ultramafic rocks from the KTB pilot hole, Bavaria. Geologische Rundschau 86, S212-S221.
78. Schumacher, J. C. (1991). Empirical ferric iron corrections: Necessity, assumptions and effects on selected geothermobarometers. MineralogicalMagazine 55, 3-18.
79. Sláma, J., Košler, J., Condon, D., Crowley, J. L., Gerdes, A., Hanchar, J.M., Horstwood, M. S. A., Morris, G. A., Nasdala, L., Norberg, N., Schaltegger, U., Schoene, B., Tubrett, M. N. & Whitehouse, M. J. (2008). Plešovice zircon - A new natural reference material for U-Pb and Hf isotopic microanalysis. Chemical Geology 30, 1-35.
80. Smith, D. & Riter, J. C. A. (1997). Genesis and evolution of low-Al orthopyroxene in spinel peridotite xenoliths, Grand Canyon field, Arizona, USA. Contributions to Mineralogy and Petrology 127, 391-404.
81. Takahashi, E. & Kushiro, I. (1983). Melting of a dry peridotite at high pressures and basalt magma genesis. American Mineralogist 68 859-879.
82. Taylor, W. R. (1998). An experimental test of some geothermometer and geobarometer formulations for upper mantle peridotites with application to the thermobarometry of fertile lherzolite and garnet websterite. Neues Jahrbuch für Mineralogie, Abhandlungen 172, 381-408.
83. Tropper, P., Konzett,Y. & Finger, F. (2005). Experimental constraints on the formation of high-P/high-T granulites in the southern Bohemian Massif. EuropeanJournal of Mineralogy 17, 343-356.
84. Tumiati, S., Thöni, M., Nimis, P., Martin, S. & Mair, V. (2003). Mantle-crust interactions during Variscan subduction in the eastern Alps (Nonsberg-Ulten zone): Geochronology and new petrological constraints. Earth and Planetary Science Letters 210, 509-526.
85. Tumiati, S., Godard, G., Martin, S., Klötzli, U. & Monticelli, D. (2007). Fluid-controlled crustal metasomatism within a high-pressure subducted mélange (Mt. Hochwart, Eastern Italian Alps). Lithos 94, 148-167.
86. Ulmer, P. & Trommsdorff, V. (1995). Serpentine stability to mantle depths and subduction-related magmatism. Nature 268, 858-861.
87. Van Roermund, H. L. M., Carswell, D. A., Drury, M. R. & Heijboer, T. C. (2001). Micro-diamonds in a megacrystic garnet-websterite pod from Bardane on the island of Fjørtoft, western Norway. Geology 30 959-962.
88. Vrána, S. (1989). Perpotassic granulites from southern Bohemia. A new rock type derived from partial melting of crustal rocks under upper mantle conditions. Contributions to Mineralogy and Petrology 103, 510-522.
89. Vrána, S. & Frýda, J. (2003). Ultrahigh-pressure grossular-rich garnetite from the Moldanubian Zone, Czech Republic. European Journal of Mineralogy 15, 43-54.
90. Vrijmoed, J. C., Van Roermund, H. L. M. & Davies, G. R. (2006). Evidence of diamond-grade ultra-high pressure metamorphism and fluid interaction in the Svartberget Fe-Ti garnet peridotite-websterite body, Western Gneiss Region, Norway. Mineralogy and Petrology 88, 381-405.
91. Winterburn, P. A., Harte, B. & Gurney, J. H. (1990). Peridotite xenoliths from the Jagersfountein kimberlite pipe: I. Primary and primary metasomatic mineralogy. Geochimica et Cosmochimica Acta 54, 329-341.
92. Witt-Eickshen, G. & Seck, H. A. (1991). Solubility of Ca and Al in orthopyroxene from spinel peridotite: An improved version of an empirical geothermometer. Contributions to Mineralogy and Petrology 106, 431-439.
93. Zaccarini, F., Stumpel, E. F. & Garuti, G. (2004). Zirconolite and Zr-Th-U minerals in chromitites of the Finero complex, Western Alps, Italy: Evidence for carbonatite-type metasomatism in a subcontinental mantle plume. Canadian Mineralogist 42, 1825-1845.
94. Zanetti, A., Mazzucchelli, M., Rivalenti, G. & Vannucci, R. (1999). The Finero phlogopite-peridotite massif: An example of subduction-related metasomatism. Contributions to Mineralogy and Petrology 134, 107-122.