 |
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
 |
|
|||||||||||||||||||||
 |
 |
 |
 |
 |
 |
 |
 |
 |
|
|||||||||||||
 |
 |
 |
 |
 |
 |
|
||||||||||||||||
 |
 |
 |
 |
|
||||||||||||||||||
 |
 |
 |
 |
|
||||||||||||||||||
 |
 |
 |
|
|||||||||||||||||||
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|
|||||||||||||||||||||
|
|
|
|
|
|
|
|
|
|
|||||||||||||
|
|
|
|
|
|
|
||||||||||||||||
|
|
|
|
|
||||||||||||||||||
|
|
|
|
|
||||||||||||||||||
|
|
|
|
|||||||||||||||||||
CdCO3
Hexagonal
Otavite, a cadmium carbonate mineral, was reported in The Picking Table (Volume 28, #2, page 3) as a quotation from correspondence from Dr. Sidney Williams. He stated that otavite occurred as a “botryoidal white crust along an open fracture cutting massive zincite that hosted scattered grains of franklinite. The crust was 2-5 mm thick and the zincite immediately adjacent to it did not appear corroded. Identification was by X-ray diffraction data and XES (to verify the high Cd/Zn ratio). I believe this is an old specimen judging by its patina.” Otavite has not been seen by the writer.
 |
|
|||
|
|
||||
|
||||
| Copyright © 1995 by Pete J. Dunn |
Website
by Herb Yeates
|
|||
|
|
|
|||
|
Link
to homepage
|
||||
|
This
page created: January 11, 2001 |
||||
|
|
|
|||
