Water-saturated and undersaturated melting relations in a Paricutin andesite and an estimate of water content in the natural magma

Author:

Eggler David H.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference23 articles.

1. Bence, A. E., Albee, A. L.: Empirical correction factors for the electron microanalysis of silicates and oxides. J. Geol. 76, 382?403 (1968).

2. Boettcher, A. L., Wyllie, P. J.: Melting of granite with excess water to 30 kilobars pressure. J. Geol. 76, 235?244 (1968).

3. Bryan, W. B.: Materials balance in igneous rock suites. Carnegie Inst. Wash. Year Book 67, 241?243 (1969).

4. Burnham, C. W., Davis, N. F.: The role of H2O in silicate melts I. P-V-T relations in the system NaAlSi3O8-H2O to 10 kilobars and 1000° C. Am. J. Sci. 270, 54?79 (1971).

5. 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. 267-A (Schairer volume), 70?95 (1969).

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