[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