Sapphirine-bearing assemblages in the system MgO-Al2 O3-SiO2: A continuing ambiguity

European Journal of Mineralogy

Volumn 20, Issue 5, 2008, Pages 721-734

  Podlesskii, Konstantin K ^a   Aranovich, Leonid Y ^a,b   Gerya, Taras V ^c   Kosyakova, Natalia A ^a  

^a INSTITUTE OF EXPERIMENTAL MINERALOGY   (Russian Federation)

^b INSTITUTE OF GEOLOGY OF ORE DEPOSITS   (Russian Federation)

^c ETH ZURICH   (Switzerland)

Author keywords

MgO Al2O3 SiO2; Sapphirine; Thermodynamic data; Ultrahigh temperature metamorphism

Indexed keywords

ALUMINA; ALUMINUM OXIDE; MAGNESIA; OXIDE MINERALS; SILICA; TEMPERATURE;

ENDMEMBERS; FORSTERITES; NON IDEALS; SAPPHIRINE; THERMOCALC; THERMODYNAMIC DATA; ULTRAHIGH TEMPERATURE;

SILICATE MINERALS;

EXPERIMENTAL MINERALOGY; MAGNESIUM; P-T CONDITIONS; SAPPHIRINE; SOLID SOLUTION; THERMODYNAMIC PROPERTY; ULTRAHIGH TEMPERATURE METAMORPHISM;

EID: 56849107823     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2008/0020-1870     Document Type: Article

References (95)

1. Ackermand, D., Seifert, F., Schreyer, W. (1975): Instability of sapphirine at high pressures. Contrib. Mineral. Petrol., 50, 79-92.
2. 3 in enstatite at high temperatures and 1-5 kb water pressure. Contrib. Mineral. Petrol., 34, 272-287.
3. Aranovich, L. Y. & Kosyakova, N.A. (1987): The cordierite = orthopyroxene + quartz equilibrium: laboratory data on and thermodynamics of ternary Fe-Mg-Al orthopyroxene solid solutions. Geochemistry Int., 24, 111-131.
4. Aranovich, L.Y. & Podlesskii, K.K. (1989): Geothermobarometry of high-grade metapelites: simultaneously operating reactions. in "Evolution of Metamorphic Belts", R.A. Cliff, B.W.D. Yardley, J.S. Daly, eds. Geol. Soc. London Spec. Publ., 43, 45-62.
5. 6 at 10-25 kbar. Contrib. Mineral. Petrol., 61, 251-265.
6. Asami, M., Grew, E.S., Makimoto, H. (2007): Relict sapphirine + kyanite and spinel + kyanite associations in pyropic garnet from the eastern Sør Rondane Mountains, East Antarctica. Lithos, 93, 107-125.
7. Baldwin, J.A., Powell, R., Williams, M.L., Goncalves, P. (2007): Formation of eclogite, and reaction during exhumation to midcrustal levels, Snowbird tectonic zone, western Canadian Shield. J. metamorphic Geol., 25, 953-974.
8. 2 system. Eur. J. Mineral., 10, 1283-1293.
9. Barbier, J. & Hyde, B.G. (1988): Structure of sapphirine: its relation to the spinel, clinopyroxene and β-gallia structures. Acta Crystallogr., B44, 373-377.
10. 2. Contrib. Mineral. Petrol., 126, 1-24.
11. Bishop, F.C. & Newton, R.C. (1975): The composition of low pressure synthetic sapphirine. J. Geol., 83, 511-517.
12. Boyd, F.R. & England, J.L. (1959): Pyrope. Carnegie Inst. Wash. Year Book, 58, 83-87.
13. 3: an experimental study. Am. Mineral., 92, 735-747.
14. Burzo, E. (2004): Sapphirine and related silicates. in "Magnetic properties of non-metallic inorganic compounds based on transition elements: orthosilicates", H.P.J. Wijn, ed. Landolt-Bornstein-Group III Condensed Matter, vol. 27, subvol. II (Orthosilicates), Springer-Verlag, 339-354.
15. 2 from high temperature solution calorimetry. Geochim. Cosmochim. Acta, 39, 1487-1497.
16. 2. Contrib, Mineral. Petrol., 36, 49-62.
17. Christy, A.G. (1989a): The effect of composition, temperature and pressure on the stability of the 1Tc and 2M polytypes of sapphirine. Contrib. Mineral. Petrol., 103, 203-215.
18. Christy, A.G. (1989b): A short-range interaction model for polytypism and planar defect placement in sapphirine. Phys. Chem. Minerals, 16, 343-351.
19. -1 exchange. Am. Mineral., 89, 327-338.
20. 2O and comparison with naturally occurring beryllian sapphirine and khmaralite. Part 1: experiments, TEM, and XRD. Am. Mineral., 87, 1104-1112.
21. 3 isopleths of enstatite in the spinel field. Contrib. Mineral. Petrol., 66, 189-201.
22. Das, K., Dasgupta, S., Miura, H. (2001): Stability of osumilite coexisting with spinel solid solution in metapelitic granulites at high oxygen fugacity. Am. Mineral., 86, 1423-1434.
23. Das, K., Dasgupta, S., Miura, H. (2003): An experimentally constrained petrogenetic grid in the silica-saturated portion of the system KFMASH at high temperatures and pressures. J. Petrol., 44, 1055-1075.
24. Das, K., Fujino, K., Tomioka, N., Miura, H. (2006): Experimental data on Fe and Mg partitioning between coexisting sapphirine and spinel: an empirical geothermometer and its application. Eur. J. Mineral., 18, 49-58.
25. Doroshev, A.M. & Malinovsky, I.Yu. (1974): Upper pressure limit of stability of sapphirine. Dokl. Akad. Nauk SSSR, 219, 136-138.
26. 2O. Am. Mineral., 51, 353-380.
27. 2-H2O (MASH) at 800 °C and 10 kbar water pressure, and the influence of FeNaCa impurities. Contrib. Mineral. Petrol., 136, 184-191.
28. 2. J. Am. Ceram. Soc., 33, 73-84.
29. Friend, C.R.L. (1982): Al-Cr substitution in peraluminous sapphirines from Bjornesund area, Fiskenæsset region, southern West Greenland. Mineral. Mag., 46, 323-328.
30. 2. J. Geol., 102, 97-109.
31. 2. Contrib. Mineral. Petrol., 85, 186-196.
32. 2. Exp. Geosci., 5, N2, 24-26.
33. Gerya, T.V., Podlesskii, K.K., Perchuk, L.L., Swamy, V., Kosyakova, N.A. (1998): Equation of state of minerals for thermodynamic databases used in petrology. Petrology, 6, 511-526.
34. Gerya, T.V., Perchuk, L.L., Podlesskii, K.K. (2004a): Database and mineral thermobarometry program "GEOPATH". in "Experimental mineralogy: some results on the Century's Frontier", V.A. Zharikov & V.V. Fed'kin, eds. Nauka, Moscow, 2, 188-206 (in Russian).
35. Gerya, T.V., Podlesskii, K.K., Perchuk, L.L., Maresch, W.V. (2004b): Semi-empirical Gibbs free energy formulations for minerals and fluids for use in thermodynamic databases of petrological interest. Phys. Chem. Minerals, 31, 429-455.
36. 2. Eur. J. Mineral., 9, 175-223.
37. Grew, E.S., Chernosky, J.V., Werding, G., Abraham, K., Marquez, N., Hinthorne, J.R. (1990): Chemistry of kornerupine and associated minerals, a wet chemical, ion microprobe, and X-ray study emphasizing Li, Be, B and F contents. J. Petrol., 31, 1025-1070.
38. Grew, E.S., Yates, M.G., Romanenko, I.M., Christy, A.G., Swihart, G.H. (1992): Calcian, borian sapphirine from the serendibite deposit at Johnsburg, NY, USA. Eur. J. Mineral., 4, 475-485.
39. Grew, E.S., Pertsev, N.N., Yates, M.G., Christy, A.G., Marquez, N., Chernosky, J.V. (1994): Sapphirine + forsterite and sapphirine + humite group minerals in an ultra-magnesian lens from Kuhi-Lal, SW Pamirs, Tajikistan: are these assemblages forbidden? J. Petrol., 35, 1275-1293.
40. Grew, E.S., Yates, M.G., Shearer, C.K., Haggerty, J.J., Sheraton, J.W., Sandiford, M. (2006): Beryllium and other trace elements in paragneisses and anatectic veins of the ultrahigh-temperature Napier Complex, Enderby Land, East Antarctica: the role of sapphirine. J. Petrol., 47, 859-882.
41. Harley, S.L. (1998): On the occurence and characterization of ultrahigh-temperature crustal metamorphism. in "What Drives Metamorphism and Metamorphic Reactions?" P.J. Treloar & P.J. O'Brien, eds. Geol. Soc. London Spec. Publ., 138, 81-107.
42. Harley, S.L. (2008): Refining the P-T records of UHT crustal metamorphism. J. metamorphic Geol., 26, 125-154.
43. Harley, S.L. & Christy, A.G. (1995): Titanium-bearing sapphirine in a partially melted aluminous granulite xenolith, Vestfold Hills, Antarctica: geological and mineralogical implications. Eur. J. Mineral., 7, 637-653.
44. 2. Carnegie Inst. Wash., Year Book, 71, 421-427.
45. Hensen, B.J. (1986): Theoretical phase relations involving cordierite and garnet revisited: the influence of oxygen fugacity on the stability of sapphirine and spinel in the system Mg-Fe-Al-Si-O. Contrib. Mineral. Petrul., 92, 362-367.
46. 2. Contrib. Mineral. Petrol., 30, 72-83.
47. Hensen, B.J. & Green, D.H. (1971): Experimental study of the stability of cordierite and garnet in pelitic compositions at high pressures and temperatures: I. Compositions with excess alumino-silicate. Contrib. Mineral. Petrol., 33, 309-330.
48. Hensen, B.J. & Harley, S.L. (1990): Graphical analysis of P-T-X relations in granulite facies metapelites. in "High-temperature metamorphism and crustal anatexis", J.R. Ashworth & M. Brown, eds. Unwin Hyman, United Kingdom, 19-56.
49. 2. Contrib. Mineral. Petrol., 84, 84-90.
50. IV ordering in monoclinic sapphirine. Contrib. Mineral. Petrol., 68, 357-368.
51. Higgins, J.B., Ribbe, P.H., Herd, R.K. (1979): Sapphirine. I. Crystal chemical contributions. Contrib. Mineral. Petrol., 68, 349-356.
52. Holland, T.J.B. & Powell, R. (1998): An internally-consistent thermodynamic dataset for phases of petrological interest. J. metamorphic Geol., 16, 309-343.
53. Hollis, J.A. & Harley, S.L. (2003): Alumina solubility in orthopyroxene coexisting with sapphirine and quartz. Contrib. Mineral. Petrol., 144, 473-483.
54. 2 systems. J. Phase Equilib., 25, 329-345.
55. Kelsey, D.E. (2008): On ultrahigh-temperature crustal metamorphism. Gondwana Res., 13, 1-29.
56. 2O for sapphirine-quartz-bearing mineral assemblages. J. metamorphic Geol., 22, 559-578.
57. Kiseleva, I.A. & Topor, N.D. (1975): High-temperature heat-capacity of sapphirine (in Russian). Geokhimiya, 2, 312-315.
58. 2 at 2.0 GPa: applications to basalt fractionation, eclogites, and igneous sapphirine. J. Petrol., 41, 3-20.
59. 2O at 1.1 GPa. J. Petrol., 45, 1339-1368.
60. Malinovsky, I.Yu. & Doroshev, A.M. (1975): Low-pressure boundary of the stability field of pyrope: Experimental studies in mineralogy (in Russian), Akad. Nauk SSSR, Novosibirsk, 95-100.
61. Merlino, S. (1980): Crystal structure of sapphirine 1Tc. Z. Kristallogr., 151, 91-100.
62. Menchi, A.M. & Scian, A.N. (2005): Mechanism of cordierite formation obtained by the sol-gel technique. Materials Lett., 59, 2664-2667.
63. 2 system at 3.0 GPa: the aluminous pyroxene thermal divide and high-pressure fractionation of picritic and komatiitic magmas. J. Petrol., 39, 3-27.
64. Moore, P.B. (1969): The crystal structure of sapphirine. Am. Mineral., 54, 31-49.
65. Newton, R.C. (1972): An experimental determination of the high-pressure stability limits of magnesian cordierite under wet and dry conditions. J. Geol., 80, 398-420.
66. Newton, R.C. (1995): Simple-system mineral reactions and high-grade meta-morphic fluids. Eur. J. Mineral., 7, 861-881.
67. Newton, R.C., Charlu, T.V., Kleppa, O.J. (1974): A calorimetric investigation of the stability of anhydrous magnesian cordierite with application to granulite facies metamorphism. Contrib. Mineral. Petrol., 44, 295-311.
68. Nogteva, V.V, Kolesnik, Y.N., Paukov, I.E. (1974): Low-temperature heat-capacity and thermodynamic properties of sapphirine (in Russian). Geokhimiya, 6, 820-829.
69. Ouzegane, K., Guiraud, M., Kienast, J.R. (2003): Prograde and retrograde evolution in high-temperature corundum granulites (FMAS and KFMASH systems) from the In Ouzzal terrane (NW Hoggar, Algeria). J. Petrol., 44, 517-545.
70. 2 at 1000-1300 °C and high pressure. Am. Mineral., 68, 355-364.
71. 2 at 15-40 kbar and 900-1600 °C. Contrib. Mineral. Petrol., 78, 99-109.
72. 2. Bochumer Geol. Geotech. Arb., 44, 146-151.
73. 2. Terra Abstracts, 8, Suppl. 1, 51.
74. Mg relations in aluminous granulites. Exp. Geosci., 6, 1, 22-23.
75. Podlesskii, K.K. (2003): Hypersthene in assemblage with sillimanite and quartz as an indicator of metamorphic conditions. Trans. (Doklady) Rus. Acad. Sci./Earth Sci. Sec., 389, 248-251.
76. Powell, R. & Holland, T.J.B. (2008): On thermobarometry. J. metamorphic Geol., 26, 155-179.
77. Sabau, G., Alberico, A., Negulescu, E. (2002): Peraluminous sapphirine in retrogressed kyanite-bearing eclogites from the South Carpathians: status and implications. Int. Geol. Rev., 44, 859-876.
78. 2+-Mg exchange thermometer: implication for constraints on P-T condition of Howard Hills, Napier Complex, East Antarctica. Gondwana Res., 9, 398-408.
79. 2O at pressures between 10 and 25 kbar. Carnegie Inst. Wash., Year Book, 66, 380-392.
80. Schreyer, W. (1968): Stability of sapphirine. Carnegie Inst. Wash., Year Book, 67, 389-392.
81. Schreyer, W. & Abraham, K. (1975): Peraluminous sapphirine as a metastable reaction product in kyanite-gedrite talc shist from Sar e Sang, Afghanistan. Mineral. Mag., 40, 171-180.
82. 2. Carnegie Inst. Wash., Year Book, 60, 144-147.
83. 2. J. Petrol., 2, 324-406.
84. 2O. Am. J. Sci., 267A, Schairer volume, 407-443.
85. 2O at high pressures. Am. J. Sci., 267, 371-388.
86. 2O at pressures up to 30 kb. Phys. Earth Planet. Interiors, 3, 422-430.
87. Schreyer, W. & Yoder, H.S. (1960): Instability of anhydrous Mg-cordierite at high pressure. Carnegie Inst. Wash., Year Book, 59, 90-91.
88. Schreyer, W., Abraham, K., Behr, H.J. (1975): Sapphirine and associated minerals from the kornerupine rock of Waldbeim Saxony. N. Jb. Mineral. Abh., 126, 1-27.
89. Schreyer, W., Horrocks, P.C., Abraham, K. (1984): High-magnesium staurolite in a sapphirine-garnet rock from the Limpopobelt, South Africa. Contrib. Mineral. Petrol., 86, 200-207.
90. 2O. J. Geol., 82, 173-204.
91. Sheng, Y.J., Hutcheon, I.D., Wasserburg, G.J. (1991): Origin of plagioclase-olivine inclusions in carbonaceous chondrites. Geochim. Cosmochim. Acta, 55, 581-599.
92. Shu, C., Mingxia, X., Cailou, Z., Jiaqi, T. (2002): Fabrication of cordierite powder from magnesium-aluminum hydroxide and sodium silicate: its characteristics and sintering. Materials Res. Bull., 37, 1333-1340.
93. Simon, G. & Chopin, C. (2001): Enstatite-sapphirine crack-related assemblages in ultrahigh-pressure pyrope megablasts, Dora-Maira massif, western Alps. Contrib. Mineral. Petrol., 140, 422-440.
94. Steffen, G., Seifert, F., Amthauer, G. (1984): Ferric iron in sapphirine: a Mössbauer spectroscopic study. Am. Mineral., 69, 339-348.
95. 2O (MASH). Eur. J. Mineral., 6, 67-75.