Thermal stability of Al-Fe epidote as a function of $$f_{{\text{o}}_{\text{2}} } $$ and Fe content-Reference-Cited by-同舟云学术

Thermal stability of Al-Fe epidote as a function of $$f_{{\text{o}}_{\text{2}} } $$ and Fe content

Published:1972 Issue:4 Volume:37 Page:307-340
ISSN:0010-7999
Container-title:Contributions to Mineralogy and Petrology
language:en
Short-container-title:Contr. Mineral. and Petrol.

Author:

Holdaway M. J.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00371011.pdf

Reference62 articles.

1. Boettcher, A. L.: The system CaO-Al2O3-SiO2-H2O at high pressures and temperatures J. Petrol. 11, 337?379 (1970).

2. Brown, E. H.: The greenschist facies in part of eastern Otago, New Zealand. Contr. Mineral. and Petrol. 14, 259?292 (1967).

3. Burnham, C. W.: Lattice constant refinement. Carnegie Inst. Wash. Year Book 61, 132?135 (1962).

4. Burnham, C. W., Holloway, J. R., Davis, N. F.: Thermodynamic properties of water to 1000° C and 10,000 bars. Geol. Soc. Am. Spec. Paper 132, 96 p. (1969).

5. Burns, R. G., Strens, R. G. J.: Structural interpretation of polarized absorption spectra of the Al-Fe-Mn-Cr epidotes. Mineral. Mag. 36, 204?226 (1967).

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