Phase relations of osumilite and dehydration melting in pelitic rocks: A simple thermodynamic model for the KFMASH system

Contributions to Mineralogy and Petrology

Volumn 124, Issue 3-4, 1996, Pages 383-394

  Holland, T J B ^a   Babu, E V S S K ^a   Waters, D J ^b  

^a Department of Earth Sciences ^*  (United Kingdom)

^b UNIVERSITY OF OXFORD   (United Kingdom)

Author keywords

[No Author keywords available]

Indexed keywords

DEHYDRATION MELTING; KFMASH SYSTEM; OSUMILITE; PELITIC ROCK; PHASE RELATIONS; THERMODYNAMICS;

EID: 0030391682     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s004100050198     Document Type: Article

References (43)

1. Arima M, Gower CF (1991) Osumilite-bearing granulites in the eastern-Grenville province, Eastern Labrador, Canada: mineral paragenesis and metamorphic conditions. J Petrol 32:29-61
2. Audibert N, Bertrand P, Hensen BJ, Kienast JR, Ouzegane KH (1993) Cordierite-K-feldspar-quartz-orthopyroxene symplectite from southern Algeria: new evidence for osumilite in high-grade metamorphic rocks. Mineral Mag 57:354-357
3. 2O at high pressure and temperature. J Metamorphic Geol 13:331-344
4. Berg JH (1977) Regional geobarometry in the contact aureoles of the anorthositic Nain Complex, Labrador. J Petrol 18:399-430
5. Berg JH, Wheeler EP II (1976) Osumilite of deep-seated origin in the contact aureole of the anorthositic Nain complex, Labrador. Am Mineral 61:29-37
6. 2: representation, estimation, and high temperature extrapolation. Contrib Mineral Petrol 89:168-183
7. 2O solutions: a thermodynamic model for hydrous magmas. In: Sabatier G (ed) Bull Soc Fr Mineral Cristallogr Spec Issue 97, pp 223-230
8. 2O to 10 kilobars and 1000°C. Am J Science 270:54-79
9. Carrington DP, Harley SL (1995a) Partial melting and phase relations in high-grade metapelites: an experimental petrogenetic grid in KFMASH system. Contrib Mineral Petrol 120:270-291
10. Carrington DP, Harley SL (1995b) The stability of osumilite in metapelitic granulites. J Metamorphic Geol 13:613-625
11. Carrington DP, Watt GR (1995) A geochemical and experimental study of the role of K-feldspar during water-undersaturated melting of metapelites. Chem Geol 122:59-76
12. Chinner GA, Dixon PD (1973) Irish oxumilite. Mineral Mag 39:189-192
13. Ellis DJ, Sheraton JW, England RN, Dallwitz WB (1980) Osumilite-sapphirine-quartz granulites from Enderby land Antarctica - mineral assemblages and reactions. Contrib Mineral Petrol 72:123-143
14. Ghiorso MS, Sack RO (1995) Chemical mass transfer in magmatic processes. IV. A revised and internally consistent thermodynamic model for the interpretation and extrapolation of liquid-solid equilibria in magmatic systems at elevated temperatures and pressures. Contrib Mineral Petrol 119:197-212
15. Grew ES (1980) Osumilite in the granulite facies: pressure-temperature conditions of formation implied by paragenesis in the sapphirine-quartz terrain of Enderby land. Antarctica (abstract). Geol Soc Am Abstr Program 12:437-438
16. Grew ES (1982a) Osumilite in the sapphirine-quartz terrane of Enderby Land. Antarctica: implications for osumilite petrogenesis in the granulite facies. Am Mineral 67:762-787
17. Grew ES (1982b) Sapphirine, kornerupine and sillimanite + orthopyroxene in the charnockitic region of south India. J Geol Soc India 23:469-505
18. Harley SL, Hensen BJ (1990) Archaean and Proterozoic high-grade terranes of East Antarctica (40-80°E): a case study of diversity granulite facies metamorphism. In: Ashworth JR, Brown M (eds) High-temperature metamorphism and crustal anatexis. Unwin Hyman, London, pp 320-370
19. Hensen BJ (1977) The stability of osumilite in high grade metamorphic rocks. Contrib Mineral Petrol 64:196-204
20. Hensen BJ, Osanai Y (1994) Experimental study of dehydration melting of F-bearing biotite in model pelitic compositions. Mineral Mag 58A:410-411
21. Holland TJB (1989) The dependence of entropy on volume for silicate and oxide minerals: a review and a predictive model. Am Mineral 74:5-13
22. 2. J Metamorphic Geol 8:89-124
23. Holland TJB, Redfern SAT, Pawley AR (1996) Volume behaviour of hydrous minerals at high pressure and temperature. 2. Compressibilities of lawsonite, zoisite, clinozoisite and epidote. Am Mineral 81:341-348
24. Holtz F, Johannes W (1994) Maximum and minimum water contents of granitic melts: implications for chemical and physical properties of ascending magmas. Lithos 32:149-159
25. Jansen JBH, Blok RJP, Scheelings M (1985) Geothermobarometry and geobarometry in Rogaland and preliminary results from the Bamble area. S Norway. In. Tobi AC, Touret JLR (eds) The deep proterozoic crust in the north Atlantic provinces. D. Reidel Publishing Company. Amsterdam, pp 499-516
26. 2 contents of cordierite as an indicator of thermodynamic conditions of formation. Geochem Int 22(1):148-156
27. Lal RK, Ackermand D, Upadhyay H (1987) P-T-X relationships deduced from corona textures in sapphirine-spinel-quartz assemblages from Paderu. southern India. J Petrol 28:1139-1168
28. Lange RA, Carmichael ISE (1990) Thermodynamic properties of silicate liquids with emphasis on density, thermal expansion and compressibility. In: Nicholls J, Russel JK (eds) Modern methods of igneous petrology: understanding magmatic processes. (Reviews in mineralogy, 24). Mineral Soc Am, Washington, DC, pp 25-59
29. Maijer C, Jansen JBH, Wevers J, Poorter RPE (1977) Osumilite, a new mineral to Norway. Nor Geol Tidsskr 57:187-188
30. Maijer C, Andriessen PAM, Hebeda EH, Jansen JBH, Verschure RH (1981) Osumilite, an approximately 970 Ma old, high-temperature index mineral of the granulite-facies metamorphism in Rogaland, SW, Norway. Geol Mjinbouw 60:267-272
31. Miyashiro A (1956) Osumilite, a new silicate mineral, and its crystal structure. Am Mineral 41:104-116
32. 2: implications for high-temperature granulites. Eur J Mineral 5:439-445
33. 2O in magmas. Contrib Mineral Petrol 74: 211-220
34. Nowicki TE, Frimmel HE, Waters DJ (1995) The occurrence of osumilite in pelitic granulites of the Namaqualand Metamorphic Complex, South Africa. S Afr J Geol 98:191-201
35. 2O. Contrib Mineral Petrol 76:362-367
36. Pawley AR, Redfern SAT, Holland TJB (1996) Volume behaviour of hydrous minerals at high pressure and temperature. 1. Thermal expansion of lawsonite, zoisite, clinozoisite and diaspore. Am Mineral 81:335-340
37. 2O). Am Mineral 75:367-380
38. Sandiford M, Neall FB, Powell R (1987) Metamorphic evolution of aluminous granulites from Labwor Hills, Uganda. Contrib Mineral Petrol 95:217-225
39. 2O and its possible bearing on the rarity of natural osumilites. Contrib Mineral Petrol 14:343-358
40. Stebbins JF, Carmichael ISE, Moret LH (1984) Heat capacities and entropies of silicate liquids and glasses. Contrib Mineral Petrol 86:131-148
41. Tobi AC, Hermans GeAEM, Maijer C, Jansen JBH (1985) Metamorphic zoning in the high-grade Proterozoic of Rogaland-Vest Agder, SW Norway. In: Tobi AC, Touret JLR (eds) The deep Proterozoic crust in the north Atlantic provinces. D. Reidel Publishing Company, Amsterdam, pp 477-497
42. Waters DJ (1989) Metamorphic evidence for the heating and cooling path of Namaqualand granulites. In: Daly JS, Cliff RA, Yardley BWD (eds) Evolution of metamorphic belts. Geol Soc Spec Publ 43:357-363
43. Waters DJ (1991) Hercynite-quartz granulites: phase relations, and implications for crustal processes. Eur J Mineral 3:367-396