High-pressure stability of the fluor- and hydroxy-endmembers of pargasite and K-richterite-Reference-Cited by-同舟云学术

High-pressure stability of the fluor- and hydroxy-endmembers of pargasite and K-richterite

Published:1991-09 Issue:9 Volume:55 Page:2689-2694
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Foley Stephen

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference41 articles.

1. Fluorine contents of some hydrous minerals derived from upper mantle and lower crust;Aoki;Lithos,1979

2. Stable isotope, chemical and petrographic studies of high-pressure amphiboles and micas: Evidence for metasomatism in the mantle source regions of alkali basalts and kimberlites;Boettcher;Amer. J. Sci.,1980

3. Hydrothermal investigations of amphiboles;Boyd,1959

4. Calibration of a belt apparatus to 1800°C and 6 GPa;Brey;J. Geophys. Res.,1990

5. The phase equilibria of richterite and ferrorichterite;Charles;Amer. Mineral.,1975

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