OLIVINE - ORTHOPYROXENE
Matsui, Y. and Nishizawa, O. (1974): Bull. Soc. franc. Mineral. Crystallogr. 97:122-130.
OLIVINE - SPINEL
Fujii, T. (1977): Carnegie Inst. Wash. Year Book 76:563-569.
Nishizawa, O. and Akimoto, S. (1973): Contrib. Mineral. Petrol. 41:217-240.
ORTHOPYROXENE - SPINEL
Nishizawa, O. and Akimoto, S. (1973): Contrib. Mineral. Petrol. 41:217-240.
ORTHOPYROXENE - CLINOPYROXENE
Mori, T. (1978): J. Geol. 19:45-65.
ORTHOPYROXENE - CLINOPYROXENE - SPINEL - OLIVINE
Herzberg, C.T. and Chapman, N.A. (1976): Am. Min. 61:626-637.
ILMENITE - ORTHOPYROXENE and ILMENITE - CLINOPYROXENE
Bishop, F.C. (1980): Am. J. Sci. 280:46-77
ILMENITE - MAGNETITE
Powell, R. and Powell, M. (1977): Mineral. Mag. 41:257-263.
Andersen, D.J. and Lindsley, D.H. (1988): Am. Min. 73:714-726.
GARNET - OLIVINE
Kawasaki, T. and Matsui, Y. (1977): Earth Planet. Sci. Lett. 37:159-166.
O'Neill, H. and Wood, B.J. (1979): Contrib. Mineral. Petrol. 70:59-70.
GARNET - ORTHOPYROXENE
useful for peridotites, many granulites, and orthopyroxene-eclogites. Limited in accuracy and sensitivity by the small S and KD magnitudes.
Sen, S.K. and Bhattacharya, A. (1984): Contrib. Minera. Petrol. 88:64-71.
Harley, S. L. (1984): J. Petrol. 25:665-696.
Aranovich, L.Y. and Berman, R.G. (1997): Am. Mineral. 82: 345-353.
GARNET - CLINOPYROXENE
applicable, with varying degrees of uncertainty, to garnet lherzolites, garnet-clinopyroxene granulites, and eclogites.
Ellis, D.J. and Green, D.H. (1979): Contrib. Mineral. Petrol. 71:13-22.
Powell, R. (1985): J. Geol. Soc. London 142:29-38.
Krogh, E.J. (1988): Contrib. Mineral. Petrol. 99: 44-48.
Peterson, J.W. and Newton, R.C. (1989): J. Geol. 97:465-485.
Sengupta, P. et al. (1989): Contrib. Mineral. Petrol. 103: 223-227.
Green, D.H. and Adam, J. (1991): J. Metam. Geol. 9: 341-347.
Yang Ai (1994): Contrib. Mineral. Petrol. 115: 467-473.
Problems with this widely used thermometer include:
(a) crustal eclogites formed at <600 C contain ordered omphacite, and hence there may arise extra Na, Al effects on inferred T from KD in such rocks,
(b) resetting during cooling to lower T,
(c) in common with most FeMg-1 thermometers the inferred T (via KD) depends on the calculated or assumed amount of Fe3+.
GARNET - ILMENITE
Powneceby, M.I., Wall, V.J. and O'Neill, H.S.C. (1987): Contrib. Mineral. Petrol. 97:116-126.
Kohn and Spear (unpubl., GTB)
GARNET - CORDIERITE
widely used in high-grade metapelites. Problem of (OH)-content in cordierite.
Thompson, A.B. (1976): Am. J. Sci. 276:425-454.
Henson, B.J.(1977): Tectonophys. 43:73-88.
Holdaway, M.J. and Lee, S.M. (1977): Contrib. Mineral. Petrol. 63: 175-193.
Martignole, J. and Sisi, J.-C. (1981): Contrib. Mineral. Petrol. 77: 38-46.
Bhattacharya, A., Mazumdar, A.C., Sen, S.K. (1988): Am. Mineral. 73: 338-344.
GARNET - HORNBLENDE
Graham, C.M. and Powell, R. (1984): J. metam. Geol. 2:13-31.
Perchuk, L.L., et al. (1985)
Ghent, E.D. and Stout, M.Z. (1986): J. Geol. 94:736-743.
GARNET - BIOTITE
widely used in low to medium grade metapelites. Application to pelitic granulites only with caution as KD appears to be easily reset to lower T.
Ferry, J.M. and Spear, F.S. (1978): Contrib. Mineral. Petrol. 66:113-117.
Hodges, K.V. and Spear, F.S. (1982): Am. Min. 67:1118-1134.
Ganguly J. and Saxena, S.K. (1984): Am. Min. 69:88-97.
Graham, C.M. and Powell, R. (1984): J. metam. Geol. 2:13-21.
Perchuk, L.L. and Lavrent'eva, I.V. (1983): Adv. Phys. Geochem. 3:199-239, New York (Springer).
Indares, A. and Martignole, J. (1985): Am. Min. 70:272-278.
Hoinkes, G. (1986): Contrib. Mineral. Petrol. 92:393-399.
Dasgupta, S. et al. (1991): Contrib. Mineral. Petrol. 109: 130-137.
Bhattacharya, A. et al. (1992): Contrib. Mineral. Petrol. 111:87-93.
Kleemann, U. and Reinhardt, J. (1994): Europ. J. Mineral. 6: 925-941
Gessmann, C. K. et al. (1997): Am. Min. 82: 1225-1240.
Holdaway, M. J. et al. (1997): Am. Min. 82: 582-595.
Holdaway, M. J. (2001): Am. Min., in press.
Extra components can influence T estimated from KD (FeMg-1) greatly:
(a) Ca and Mn in garnet
(b) Ti, F and Cl in biotite (particularly at higher grades)
(c) Fe3+ in biotite in particular.
GARNET - CHLORITE
Dickenson, M.P. and Hewitt, D.A. (1986): Geol. Soc. Am. Abstr. Prog. 18:584.
Kohn and Spear (1989, unpubl., GTB)
Grambling, J.A. (1990): Contrib. Mineral. Petrol. 105:617-628.
GARNET - PHENGITE
Krogh, E.J. and Raheim, A. (1978)
Green and Hellmann (1982)
Hynes and Forest (1988)
MUSCOVITE - BIOTITE
Hoisch, T.D. (1989): Am. Min. 74:565-572.
BIOTITE - TOURMALINE
Colopietro and Friberg (1987)
EPIDOTE - PUMPELLYITE - CHLORITE - ACTINOLITE
Nakajima, T., Banno, S. and Suzuki, T. (1977): J. Petrol. 18:263-284.
Liou, J.G., Maruyama, S. and Cho, M. (1987): In: Frey, M., Low temperature metamorphism, p. 59-113, Glasgow (Blackie) 349 p.
