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Fe3+2(MoO4)3.8H2O?
Orhorhombic?
Ferrimolybdite, a ferric-iron molybdate hydrate mineral, was identified using X-ray methods by Parker and Smith (1984) as a yellow powdery mass in a molybdenite-bearing calcium-silicate rock. It occurred as rims around molybdenite crystals associated with powellite and in areas in the enclosing quartz. The specimen is reportedly from Sterling Hill and not Franklin.
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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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