Andrewsite
Appearance
From Wikipedia, the free encyclopedia
Andrewsite is a now discredited mineral originally reported at the Wheal Phoenix mine, near Liskeard in Cornwall. It was named for Thomas Andrews FRS, the English chemist.[1]
It has been shown to be a mixture of hentschelite and rockbridgeite, with minor chalcosiderite.[1]
References
[edit ]- ^ a b "Andrewsite: Andrewsite mineral information and data". www.mindat.org. Retrieved 2017年03月01日.
- Maskelyne, N. S. (1871) Chemical News and Journal of Industrial Science, London: 24: 99.
- Maskelyne, N. S. (1875) 'On Andrewsite and Chalkosiderite' Journal of the Chemical Society , London: 28: 586-591
- Frondel, C. (1949) 'The Dufrenite Problem', American Mineralogist : 34: 513–540.
- Palache, C., Berman, H., & Frondel, C. (1951), The System of Mineralogy of James Dwight Dana and Edward Salisbury Dana , Yale University 1837–1892, Volume II. John Wiley and Sons, Inc., New York, 7th edition, revised and enlarged, 1124 pp.: 802–803.
- Dunn, Pete J. (1990), 'Andrewsite and laubmannite formally discredited', American Mineralogist 75, 1197-1199(1990)
Stub icon
This article about a specific mineral or mineraloid is a stub. You can help Wikipedia by expanding it.