Dehydration and partial melting of tremolitic amphibole coexisting with zoisite, quartz, anorthite, diopside, and water in the system H2O-CaO-MgO-Al2O3-SiO2

Contributions to Mineralogy and Petrology

Volumn 130, Issue 3-4, 1998, Pages 379-389

  Quirion, Diane M ^a   Jenkins, David M ^a  

^a BINGHAMTON UNIVERSITY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ANORTHITE; DEHYDRATION; DIOPSIDE; PARTIAL MELTING; QUARTZ; TREMOLITE; ZOISITE;

EID: 0032450311     PISSN: 00107999     EISSN: None     Source Type: Journal    
DOI: 10.1007/s004100050372     Document Type: Article

References (26)

1. Apted MJ, Liou JG (1983) Phase relations among greenschist, epidote-amphibolite, and amphibolite in a basalt system. Am J Sci 283-A: 328-354
2. 2O assemblages. Am Mineral 81: 676-684
3. 2. J Petrol 29: 445-522
4. Berman RG (1991) Thermobarometry using multiequilibrium calculations: a new technique with petrologic applications. Can Mineral 29: 833-855
5. Chalokwu CI, Kuehner SM (1992) Mineral chemistry and thermobarometry of a southern Appalachian amphibolite with epidote + quartz symplectite. Am Mineral 77: 617-630
6. Cho M, Ernst WG (1991) An experimental determination of calcic amphibole solid solution along the join tremolite-tschermakite. Am Mineral 76: 985-1001
7. 2O system under water-excess and water-deficient conditions to 10 kb: some implications for the origin of peraluminous melts from mafic rocks. J Petrol 27: 91-121
8. Giblin LE, Blackburn WH, Jenkins DM (1993) X-ray continuum discrimination technique for the energy dispersive analysis of fine particles. Anal Chem 65: 3576-3580
9. 2O (anorthite-water) at elevated pressures and temperatures. Am Mineral 66: 1183-1188
10. Holland TJB (1980) The reaction albite = jadeite + quartz determined experimentally in the range of 600-1200°C. Am Mineral 65: 129-134
11. 2. J Metamorphic Geol 8: 89-124
12. 2O. Eur J Mineral 7: 353-362
13. 2. Am Mineral 72: 707-715
14. Jenkins DM (1988) Experimental study of the join tremolite-tschermakite: a reinvestigation. Contrib Mineral Petrol 99: 392-400
15. 2. Am J Sci 294: 593-620
16. Jenkins DM, Sherriff BL, Cramer J, Xu Z (1997) Al, Si, and Mg occupancies in tetrahedrally and octahedrally coordinated sites in synthetic aluminous tremolite. Am Mineral 82: 280-290
17. Kerrick DM, Darken LS (1975) Statistical thermodynamic models for ideal oxide and silicate solid solutions, with application to plagioclase. Geochim Cosmochim Acta 39: 1431-1442
18. Liou JG, Kuniyoshi S, Ito K (1974) Experimental studies of the phase relations between greenschist and amphibolite in a basalt system. Am J Sci 274: 613-632
19. Maruyama S, Suzuki K, Liou JG (1983) Greenschist-amphibolite transition equilibria at low pressures. J Petrol 24: 583-604
20. Moody JB, Meyer D, Jenkins JE (1983) Experimental characterization of the greenschist/amphibolite boundary in mafic systems. Am J Sci 283: 48-92
21. Newton RC (1966) Some calc-silicate equilibrium relations. Am J Sci 264: 204-222
22. Price JG (1985) Ideal site mixing in solid solutions, with an application to two-feldspar geothermometry. Am Mineral 70: 696-701
23. Schumacher R (1991) Compositions and phase relations of calcic amphiboles in epidote- and clinopyroxene-bearing rocks of the amphibolite and lower granulite facies, central Massachusetts, USA. Contrib Mineral Petrol 108: 196-211
24. Smelik EA, Jenkins DM, Navrotsky A (1994) A calorimetric study of synthetic amphiboles along the tremolite-tschermakite join and the heats of formation of magnesiohornblende and tschermakite. Am Mineral 79: 1110-1122
25. 2O between 1 and 10 kilobars. Schweiz Mineral Petrogr Mitt 47: 35-59
26. 2O to 35 KB: amphibole, talc, and zoisite dehydration and melting reactions in the silica-excess part of the system and their possible significance in subduction zones, amphibolite melting, and magma fractionation. Am J Sci 294: 1229-1289