Experimental synthesis and phase relations of phengitic muscovite from 6.5 to 11 GPa in a calcareous metapelite from the Dabie Mountains, China

Lithos

Volumn 52, Issue 1-4, 2000, Pages 51-77

  Domanik, Kenneth J ^a   Holloway, John R ^a  

^a ARIZONA STATE UNIVERSITY   (United States)

Author keywords

Experimental studies; Geochemistry; High pressure; Metamorphism; Phengite; Subduction zones

Indexed keywords

GEOCHEMISTRY; METAMORPHISM; P-T CONDITIONS; PHASE EQUILIBRIUM; PHENGITE; SUBDUCTION ZONE;

EID: 0034092531     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0024-4937(99)00084-5     Document Type: Article

References (48)

1. Akaogi M., Yusa H., Shiraishi K., Suzuki T. Thermodynamic properties of α-quartz, coesite, and stishovite and equilibrium phase relations at high pressures and temperatures. J. Geophys. Res. 100:1995;22337-22347.
2. Bebout G.E., Barton M.D. Fluid flow and metasomatism in a subduction zone hydrothermal system: Catalina Schist terrane, California. Geology. 17:1989;976-980.
3. Bebout G.E., Ryan J.G., Leeman W.P. B-Be systematics in subduction-related metamorphic rocks: characterization of the subducted component. Geochim. Cosmochim. Acta. 56:1993;2839-2849.
4. 2. J. Petrol. 29:1988;445-522.
5. 2; representation, estimation, and high temperature extrapolation. Contrib. Mineral. Petrol. 89:1985;168-183.
6. Brown T.H., Berman R.G., Perkins E.H. GEO-CALC: software package for calculation and display of pressure-temperature-composition phase diagrams using an IBM or compatible personal computer. Comput. Geosci. 14:1988;279-289.
7. Bureau H., Keppler H. Complete miscibility between silicate melts and hydrous fluids in the upper mantle: experimental evidence and geochemical implications. Earth Planet. Sci. Lett. 165:1999;187-196.
8. Burt, D.M., 1988. Vector representation of phyllosilicate compositions. In: Bailey, S.W. (Ed.), Hydrous Phyllosilicates, Reviews in Mineralogy, Vol. 19. Mineral. Soc. Am., Washington DC, pp. 561-599.
9. Domanik, K.J., 1992. The distribution of beryllium and boron in high pressure, low temperature minerals. Unpublished MS Thesis, Arizona State University.
10. Domanik, K.J., 1997. The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa. Unpublished PhD Thesis, Arizona State University.
11. Domanik K.J., Hervig R.L., Peacock S.M. Beryllium and boron in subduction zone minerals: an ion microprobe study. Geochim. Cosmochim. Acta. 57(21/22):1993;4997-5010.
12. Domanik K.J., Holloway J.R. The stability of phengitic muscovite and associated phases from 5.5 to 11 GPa: implications for deeply subducted sediments. Geochim. Cosmochim. Acta. 60(21):1996;4133-4150.
13. 2: principles and review. In: Magma Genesis; Proceedings of the American Geophysical Union Chapman Conference on Partial Melting in the Earth's Upper Mantle. Oreg. Dep. Geol. Miner. Ind. Bull. 96, pp. 15-36.
14. Gill, J., 1981. Orogenic Andesites and Plate Tectonics. Springer-Verlag.
15. Greenwood H.J. Metamorphic reactions involving two volatile components. Carnegie Inst. Washington, Year Book. 61:1962;82-85.
16. 2. In: Abelson, P.H. (Ed.), Researches in Geochemistry, Vol. II. Wiley, New York, pp. 542-547.
17. Greenwood H.J. Buffering of pore fluids by metamorphic reactions. Am. J. Sci. 275:1975;573-593.
18. Helgeson H.C., Delany J.M., Nesbitt H.W., Bird D.K. Summary and critique of the thermodynamic properties of rock-forming minerals. Am. J. Sci. 278-A:1978;1-229.
19. Howell D.G., Murray R.W. Model for continental growth and denudation. Science. 233:1986;446-449.
20. Inoue, I., Irifune, T., Yurimoto, H., Miyagi, I., 1996. Decomposition of K-amphibole at high pressures and implications for subduction zone volcanism. In: Dingwell, D.B., Mysen, B.J. (Eds.), Magmatology; the role of magmas in the evolution of the Earth. Phys. Earth Planet. Inter. 107, 221-231.
21. Irifune T., Sekine T., Ringwood A.E., Hibberson W.O. The eclogite-garnetite transformation at high pressure and some geophysical. Earth Planet. Sci. Lett. 126:1986;351-368.
22. 2) equilibria. Am. Mineral. 59:1974;729-762.
23. Kretz R. Symbols for rock-forming minerals. Am. Mineral. 68:1983;277-279.
24. Kushiro I., Satake H., Akimoto S. Carbonate-silicate reactions at high pressures and possible presence of dolomite and magnesite in the upper mantle. Earth Planet. Sci. Lett. 28:1975;116-120.
25. Li B., Rigden S.M., Liebermann R.C. Elasticity of stishovite at high pressure. Phys. Earth Planet. Inter. 96:1995;113-127.
26. Liu J., Topor L., Zhang J., Navrotsky A., Liebermann R.C. Calorimetric study of the coesite-stishovite transformation and calculation of the phase boundary. Phys. Chem. Miner. 23:1996;11-16.
27. 2O (KMASH). Lithos. 28:1992;421-434.
28. Massonne, H.J., 1995. Experimental and petrogenetic study of UHPM. In: Coleman, R.G., Wang, X. (Eds.), Ultrahigh Pressure Metamorphism. Cambridge. Univ. Press, Cambridge, pp. 33-95.
29. 2O. Neues Jahrb. Mineral., Abh. 153:1986;177-215.
30. Miyashiro, A., 1973. Metamorphism and Metamorphic Belts. Allen and Unwin.
31. Olafsson M., Eggler D.H. Phase relations of amphibole, amphibole-carbonate, and phlogopite-carbonate peridotite: petrological constraints on the asthenosphere. Earth Planet. Sci. Lett. 64:1983;305-315.
32. Ono S. Stability limits of hydrous minerals in sediment and mid-ocean ridge basalt compositions: implications for water transport in subduction zones. J. Geophys. Res. 103:1998;18253-18267.
33. 2O recycling in subduction zones. Contrib. Mineral. Petrol. 118:1994;99-108.
34. Peacock S.M., Rushmer T., Thompson A.B. Partial melting of subducting oceanic crust. Earth Planet. Sci. Lett. 121:1994;227-244.
35. Plank, T., Ludden, J.N., 1992. Geochemistry of sediments in the Argo abyssal plain at site 765: a continental margin reference section for sediment recycling in subduction zones. In: Gradstein, F.M., Ludden, J.N., et al. (Eds.), Proc. OPD, Sci. Results, Vol. 123. Ocean Drilling Program, College Station TX, pp. 167-189.
36. 2O transport and release in subduction zones: experimental constraints on basaltic and andesitic systems. J. Geophys. Res. 100:1995;22299-23314.
37. 5 Pascals) pressure and higher temperature. U.S. Geol. Surv. Bull. 1452:1978;1-456.
38. Saxena, S.K., Chatterjee, N., Fei, Y., Shen, G., 1993. Thermodynamic Data on Oxides and Silicates: An Assessed Data Set Based on Thermochemistry and High Pressure Phase Equilibrium. Springer-Verlag.
39. Schmidt M.W. Experimental constraints on recycling of potassium from subducted oceanic crust. Science. 272:1996;1927-1930.
40. Schneider M.E., Eggler D.H. Fluids in equilibrium with peridotite minerals: implications for mantle metasomatism. Geochim. Cosmochim. Acta. 50:1986;711-724.
41. Sorensen, S., 1994. Subduction-related K-Rb-Ba metasomatism of high grade melange blocks from California, USA and the Dominican Republic. SUBCON Abstr. Vol. 213-215.
42. Sorensen S.S., Grossman J.N., Perfit M.R. Phengite-hosted LILE enrichment in eclogite and related rocks: implications for fluid-mediated mass transfer in subduction zones and arc magma genesis. J. Petrol. 38:1997;3-34.
43. Stevenson, A.J., 1994. Terrigenous sedimentary input into subduction zones: sources, depositional styles, and consequences of entrainment in the subduction process. SUBCON Abstr. Vol. 49-50.
44. Tatsumi Y., Furukawa Y., Kogiso T., Yamamaka Y., Yokoyama T., Fedotov S.A. A third volcanic chain in Kamchatka: thermal anomaly at transform/convergence plate boundary. Geophys. Res. Lett. 21:1994;537-540.
45. 8. Phys. Chem. Miner. 21:1994;387-391.
46. 2: a fully hydrated analogue of topaz. Am. Mineral. 78:1993;285-297.
47. 8 hollandite. Am. Mineral. 78(5/6):1993;493-499.
48. Zhang R.Y., Liou J.G. Significance of magnesite in ultrahigh-pressure metamorphic rocks. Am. Mineral. 79:1994;397-400.