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Cu3(SO4)(OH)4
Orthorhombic
Antlerite, a copper sulfate hydroxide mineral, was found as a minor part of a thin green film composed of very fine-grained antlerite, gypsum, and brochantite, encrusting rhodonite and associated with andradite and mica from Franklin. The impure nature of the aggregate precluded the determination of any additional data; the verification was made employing X-ray powder diffraction methods.
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| Copyright © 1995 by Pete J. Dunn |
Website
by Herb Yeates
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Link
to homepage
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This
page created: January 11, 2001 |
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