Experimental calibration of the partitioning of Fe and Mg between biotite and garnet

Author:

Ferry J. M.,Spear F. S.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference15 articles.

1. Burnham, C.W.: Lattice constant refinement. Carnegie Inst. Washington Yearbook 61, 132?135 (1963)

2. Chinner, G.A., Boyd, F. R., England, J.L.: Physical properties of garnet solid solutions. Carnegie Inst. Washington Yearbook 59, 76?78 (1960)

3. Dallmeyer, R.D.: The role of crystal structure in controlling the partitioning of Mg and Fe2+ between coexisting garnet and biotite. Am. Mineralogist 59, 201?203 (1974)

4. Eugster, H.P., Albee, A.L., Bence, A.E., Thompson, J.B., Jr., Waldbaum, D.R.: The two-phase region and excess mixing properties of paragonite-muscovite crystalline solutions. J. Petrol. 13, 147?179 (1972)

5. Eugster, H.P., Skippen, G.B.: Igneous and metamorphic reactions involving gas equilibria. In: Researches in geochemistry (P.H. Abelson, ed.), Vol. 2, pp. 377?396. New York: John Wiley 1967

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