Theoretical phase relations involving cordierite and garnet in the system MgO-FeO-Al2O3-SiO2

Author:

Hensen B. J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference19 articles.

1. Barker, F.: Cordierite-garnet gneiss and associated microcline-rich pegmatite at Sturbridge, Massachusetts and Union, Connecticut. Am. Mineralogist 47, 907?918 (1962).

2. Best, M. G., Weiss, L. E.: Mineralogical relations in some pelitic hornfelses from the southern Sierra Nevada. Am. Mineralogist 49, 1240?1266 (1964).

3. Burnham, C. W., Holloway, J. R., Davis, N. F.: The specific volume of water in the range 1,000?8,900 bars, 20°?900° C. Am. J. Sci. Schairer Vol., 70?95 (1969).

4. Goldschmidt, V. M.: Die Kontaktmetamorphose im Kristianagebiet. Kristiana Vidensk Skr., Math.-Naturv. Kl. 11 (1911).

5. Grant, J. A.: Partial melting of common rocks as a possible source of cordierite-anthophyllite bearing assemblages. Am. J. Sci. 266, 908?931 (1968).

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