Experimental evidence on phlogopitic mantle metasomatism induced by phengite dehydration

European Journal of Mineralogy

Volumn 15, Issue 4, 2003, Pages 641-647

  Wunder, Bernd ^a   Melzer, Stefan ^b  

^a GFZ GERMAN RESEARCH CENTRE FOR GEOSCIENCES   (Germany)

^b Delft University of Technology Corus Research Development and Technology   (Netherlands)

Author keywords

Experimental study; LILE fractionation; Mantle metasomatism; Phengite; Phlogopite

Indexed keywords

BINARY ALLOYS; CESIUM ALLOYS; DEHYDRATION; MICA; OLIVINE; POTASSIUM ALLOYS; RUBIDIUM ALLOYS;

CONVERGENT PLATE BOUNDARIES; EXPERIMENTAL SIMULATIONS; EXPERIMENTAL STUDY; EXPERIMENTAL TECHNIQUES; MANTLE METASOMATISM; PHENGITE; PHLOGOPITE; PISTON-CYLINDER APPARATUS;

MINERALOGY;

DEHYDRATION; EXPERIMENTAL STUDY; FRACTIONATION; MANTLE; METASOMATISM; MICA; P-T CONDITIONS; PHENGITE; PHLOGOPITE; SUBDUCTION;

EID: 0041926333     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2003/0015-0641     Document Type: Article

References (28)

1. Colson, R.O., McKay, G.A., Taylor, L.A. (1988): Temperature and composition dependencies of trace element partitioning: Olivine/melt and low-Ca pyroxene/melt. Geochim. Cosmochim. Acta, 52, 539-553.
2. Domanik, K.J. & Holloway, J.R. (1996): The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa: Implication for deeply subducted sediments. Geochim. Cosmochim. Acta, 60, 4133-4150.
3. Feenstra, A. & Wunder, B. (2002): Dehydration of diasporite to corundite in nature and experiment. Geology, 30, 2, 119-122.
4. 2 (MAS). Eur. J. Mineral., 9, 509-518.
5. 2. Contrib. Mineral. Petrol., 85, 186-196.
6. Green, D.H. (1982): Anatexis of mafic crust and high pressure crystallization of andesite. in R.S. Thorpe (Ed.), Andesites. Wiley, London, pp. 465-487.
7. Griffin, W.L., Shee, S. R., Ryan, C.G., Win, T.T., Wyatt, B.A. (1999): Harzburgite to lherzolite and back again: metasomatic processes in ultramafic xenoliths from Wesselton kimberlite, Kimberley, South Africa. Contrib. Mineral. Petrol., 134, 232-250.
8. Harlow, G.E. & Veblen, D.R. (1991): Potassium in clinopyroxene inclusions from diamonds. Science, 251, 652-655.
9. Massonne, H.-J. & Schreyer, W. (1987): Phengite geobarometry based on limiting assemblages with K-feldspar, phlogopite, and quartz. Contrib. Mineral. Petrol., 96, 212-224.
10. Melzer, S. & Wunder, B. (2000): Island-arc basalt alkali ratios: Constraints from phengite-fluid partitioning experiments. Geology, 28, 583-586.
11. Melzer, S. & Wunder, B. (2001): K-Rb-Cs partitioning between phlogopite and fluid: experiments and consequences on the LILE signatures of island arc basalts. Lithos, 59, 69-90.
12. Modreski, P.J. & Boettcher, A.L. (1972): The stability of phlogopite and enstatite at high pressures: a model for micas in the interior of the earth. Am. J. Sci., 272, 852-869.
13. Peacock, S.M. (1990): Fluid processes in subduction zones. Science, 248, 329-337.
14. Peacock, S.M. & Wang, K. (1999): Seismic consequences of warm versus cool subduction metamorphism: Examples from southwest and northwest Japan. Science, 286, 937-939.
15. Pouchou, J.L. & Pichoir, F. (1984): Un nouveau modèle de calcul pour la microanalyse quantitative par spectroétrie de rayons. X. Rech. Aérosp., 3, 167-192.
16. Ryabchikov, I.D. & Boettcher, A.L. (1980): Experimental evidence at high pressures for potassic metasomatism in the mantle of the earth. Am. Mineral., 65, 915-919.
17. Ryan, J.G., Morris, J., Tera, F., Leeman, W.P., Tsvetkov, A. (1995): Cross-arc geochemical variations in the Kurile arc as a function of slab depth. Science, 270, 625-627.
18. Schmidt, M.W. (1996): Experimental constraints on recycling of potassium from subducted oceanic crust. Science, 272, 1927-1930.
19. Schmidt, M.W. & Poli, S. (1998): Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation. Earth Planet. Sci. Lett., 163, 361-379.
20. Sudo, A. & Tatsumi, Y. (1990): Phlogopite and K-amphibole in the upper mantle: implication for magma genesis in subduction zones. Geophys. Res. Lett., 17, 1, 29-32.
21. Tatsumi, Y. & Nakamura, N. (1986): Composition of aqueous fluid from serpentinite in subducted lithosphere. Geochem. J., 20, 191-196.
22. Velde, B. (1965): Phengite micas: Synthesis, stability, and natural occurrence. Am. J. Sci., 263, 886-913.
23. Wunder, B. & Melzer, S. (2002): Interlayer vacancy characterization of synthetic phlogopitic micas by IR spectroscopy. Eur. J. Mineral., 14, 1129-1138.
24. 2O (MSH). What about hydrous phases in subduction zones? J. Petrol., 33, 877-889.
25. 2O (MSH). Lithos, 41, 213-227.
26. Wyllie, P.T. & Sekine, T. (1982): The formation of mantle phlogopite in subduction zone hybridization. Contrib. Mineral. Petrol., 79, 375-380.
27. Zanetti, A., Mazzucchelli, M., Rivalenti, G., Vannucci, R. (1999): The Finero phlogopite-peridotite massif: an example of subduction-related metasomatism. Contrib. Mineral. Petrol., 134, 107-122.
28. Zhang, H., Menzies, M.A., Zhao, L., Lu, F., Zhou, X. (2000): Multi-phase mineral inclusions in diamonds from Fuxian and Mengyin kimberlites, Eastern China. J. Conf. Abstr,, 5(2), 1125.