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Fluorescent X-Ray Spectrographic Analyses of Amphibolite Rocks and Constituent Hornblendes

Published online by Cambridge University Press:  06 March 2019

A. A. Chodos
Affiliation:
California Institute of Technology, Pasadena, California
Celeste G. Engel
Affiliation:
U. S. Geological Survey, University of California La Jolla, California
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Abstract

Fluorescent X-ray spectrographic analyses have been made for the oxides Fe2O3 caO, MgO, K2O, TiO2, and MnO on samples of amphibolite rock. In addition, the above oxides and SiO2 and Al2O3 have been determined in a suite of constituent hornblendes from these rocks.

Classical wet chemical analyses of materials of the same minera logical composition as the samples are used to establish the working curves. This eliminates the necessity for Internal standardization or other treatment of the samples. The only sample preparation involves extremely fine grinding before analysis.

Precision of the analyses is equivalent to, or better than, that achieved by wet chemical methods.

Type
Research Article
Copyright
Copyright © International Centre for Diffraction Data 1960

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References

1. Chodos, A. A., Branco, J. J. R., and Engel, C. G., “Rock Analysis by X-Ray Fluorescence Spectroscopy,” Advances in X-Ray Analysts, Vol. 1, University of Denver, Plenum Press, New York, 1960, p. 315.Google Scholar
2. Chodos, A. A. and Engel, C. G., “Fluorescent X-Ray Spectrographic Analyses of Amphibolite Rocks,” Am. Mineral, 1961, in press.Google Scholar
3. Fairbairn, H. W., “A Cooperative Investigation of Precision and Accuracy in Chemical, Spectrochemical, and Modal Analysis of Silicate Rocks,” U.S. Geol. Survey Bull., 980, 1951.Google Scholar
4. Engel, A. E. J. and Engel, C. G., ‘Progressive Metamorphlsm andGranitization of the Major Paragneiss, Northwest Adirondack Mountains, New York, Part I: Total Rock,’ Bull. Geol. Soc. Am., Vol. 69, November, 1958, p. 1369.Google Scholar
5. Engle, A. E. J. and Engel, C. G., ‘Progressive Metamorphism and Granitization of the Major Paragneiss, Northwest Adirondack Mountains, New York, Part II: Mineralogy,’ Bull. Geol. Soc. Am., Vol. 71, January, 1960, p. 1.Google Scholar
6. Stevens, R. E. et al., “Second Report on a Cooperative Investigation of the Composition of Two Silicate Rocks,’ U. S. Geol. Survey BulL, 1113, 1960.Google Scholar