The stability of pyrope-grossular garnet with excess silica

Author:

Hensen B. J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference16 articles.

1. Kushiro, I., Yoder, H.S.: Anorthite-forsterite and anorthite-enstatite and their bearing on the basalt-eclogite transformation. J. Petrol. 7, 337?362 (1966)

2. Kushiro, I.: Clinopyroxene solid solutions formed by reactions between diopside and plagioclase at high pressures. Mineral. Soc. Am. Spec. Papers 2, 179?191 (1969)

3. Green, T.H.: The diopside-kyanite join at high pressures and temperatures. Lithos 2, 334?341 (1969)

4. Emslie, R.T.: Subsolidus reactions in the system enstatite-anorthite at 1,212 °C and pressures up to 20 kb. Carnegie Inst. Wash. Year book 69, 152?154 (1971)

5. Hensen, B.J.: The relative stability of garnet granulite and kyanite eclogite. Carnegie Inst. Wash. Year book 71, 426?427 (1972)

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