[1] Andeson,G.M.and Burnham,C.W.,1983, Feldspar solubility and the transport of alumium under metamorphic conditions,Amer. J. Sci.. 283-A. 283-297. [2] Brady, J. B.,1983, Intergranular diffusion in metamorphic tacks, Amer. J. Sci.,283-A, 181-200. [3] Cho, Moonsup and Fawcett, J. J.,1986, A Kinetic study of clinochlore and its high temperature equivalent foraterite-cordierite-spinel at 2 Kbar water pressure,Amer,. Mineral, 71,68-77. [4] Cygan, R. T. and Lasaga,A .C.,1985, Selt-diffusion of magnesium in garnet at 750 to 900°C,Amer. J. Sci.,285,328-350. [5] Elphick,S. C.,Gauguly, J. and loomis, T. P.,1985, Experimental defermination of catian diffusivites in aluminosilicate garnets. I. Experimental methods and interdiffusion data, Contrib.Mineral. Petrol.,90, 35-44. [6] Flowers G. C. and Helgeson, H. C.,1983,Equihbrium and mass transfer during progressive metamorphism of siliceous dolomites,Amer J.Sci.,283,230-286. [7] Joesten, R.,1983, Grain growth and grain boundary diffusion in quartz from the Christmas Mountains (Texas) contract aureole, Amer J. Sci.,,283-A,233-254. [8] Loomis, A. C.,1983, Geospedometry: An extension of geothermometry, in: Advances in physical Geochemistry V.3(ed. S.K.Saxena),PP. 81-114, Springer-Verlag. [9] Loomis, T. P.,1983, Compositional zoning of crystals:A record of growth and reaction history, in:Advances to Physical Geochemistry v. 3 (ad S. K. saxena), pp.1-60, Springer-Verlag. [10] Loomis,T. P.,Ganguly,J, and Elphick, S. C.,1985, Experimental determimation of catiom diffusivities in aluminosilicate garnets: II Multicomponent simulation and tracer diffusion coefficient, contrib. Mineral Petrol. 90,45-51. [11] Matthews, A.,1985, Kinetics and mechanisms of the reaction of zoisite to anorthite under hydrothermal conditions: reaction phenomenology away from the equilibrium region, Contrib. Mineral. Petrol. 82, 360-370 [12] Mueller, R. F. and Saxena, S. K.,1977,chemical petrology, New York, Spring-Verlag. [13] Ridley, J. and Thompson , A. B.,1986, The role of mimeral Kinetics in the development of metamorphic microtextures, in advances in physical Geochemistry, V. 5, (eds J. V. Walther and B. J. Wood) pp154-193,springer-Verlag. [14] Tanner, S. B.,Kerrick, D. M. and Lasaga, A. C.,1985, Experimental Kinetics study of the reaction calcite+quartz=Wollastonite+carbon dioxide, from, to 3 Kllobars and 500 to 850 ℃,Amer. J. Sci.,285, 577-620 [15] Traey , R. J. and Mclellan , E. L.,1985, A natural example of the Kinetic controls of compositional and textural equilibtation,in:Advances in physical Geochemistry, V. 4 (eds. A. B. Thompson and D. C. Rubie),pp118-137, Springer-Verlag. [16] Walther, J. V. and wood, B. J.,1989, Rate and mechanism in prograde metamorphism, Contrib. Mineral.petrol.,88,246-259 [17] Walther, J. V. and wood, B. J.,1986, Mineral-fluid reaction rates,in: Advances in physical Geochemistry, V.S(eds. J. V. Walther and B. J. wood), pp199-212, Springer-Verlag [18] Winkler, H. G. F.,1976, Petrogenesis of metamerphic rocks.Lth ed, New York, springer-Verlag. [19] 董申保,变质实验岩石学和变质反应,当代地质科学动向(张炳主编),地质出版社,1987, 122-124页 [20] 李仲,李继亮,近代地质学(译文),国外地质,1989年第一期 |