Hydrothermal Melting Curves in Silicate–Water Systems at Pressures greater than 10 Kilobars-Reference-Cited by-同舟云学术

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Hydrothermal Melting Curves in Silicate–Water Systems at Pressures greater than 10 Kilobars

Published:1967-11 Issue:5115 Volume:216 Page:572-573
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

BOETTCHER A. L.,WYLLIE P. J.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/216572a0.pdf

Reference4 articles.

1. Barth, T. F. W., in Theoretical Petrology (Wiley and Sons, 1962).

2. Smith, F. G., in Physical Geochemistry (Addison-Wesley, 1963).

3. Kadik, A. A., and Khitarov, N. I., Geochemistry, No. 10, 917 (1963).

4. Peters, Tj., Luth, W. C., and Tuttle, O. F., Amer. Mineral., 51, 736 (1966).

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1. Phase Relationships of I-Type Granite With H20 to 35 Kilobars: The Dinkey Lakes Biotite-Granite From the Sierra Nevada Batholith;1989, Granites and Rhyolites;2013-12-20

2. The Nature of the Crust of the Earth, with Special Emphasis on the Role of Plagioclase;Geophysical Monograph Series;2013-03-15

3. Hydrothermal experiments on alteration of Ca-Al-rich inclusions (CAIs) in carbonaceous chondrites: implication for aqueous alteration in parent asteroids;Geochimica et Cosmochimica Acta;1998-11

4. Phase relationships of I-type granite with H2O to 35 kilobars: The Dinkey Lakes biotite-granite from the Sierra Nevada Batholith;Journal of Geophysical Research: Solid Earth;1981-11-10

5. Water and carbon dioxide in magmatic melts and peculiarities of the melting process;Contributions to Mineralogy and Petrology;1973

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