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Compact chlorite associated with lizardite from New South Wales, Australia
Published online by Cambridge University Press: 14 March 2018
Summary
Segregations of compact chlorite from ultramafic belts in New South Wales have been examined using chemical, X-ray, differential thermal, and electronprobe techniques. The chlorites vary from pennine to sheridanite. Some segregations occupy the central zone in metasomatic sequences of altered chromite, chlorite, and lizardite; but others may have formed at junctions of serpentinite and rodingite.
- Type
- Research Article
- Information
- Mineralogical magazine and journal of the Mineralogical Society , Volume 36 , Issue 282 , June 1968 , pp. 825 - 831
- Copyright
- Copyright © The Mineralogical Society of Great Britain and Ireland 1968
References
Thayer, (T. P.), 1956. Mineralogy and geology of chromium. In Chromium, Amer. Chem. Soc. Mon. 132, p. 14.Google Scholar
Webster, (R.), 1962. Gems, their sources, descriptions and identification. Butterworths, London.Google Scholar