Abstract
Irradiation-induced colour in amazonite can develop only in K-feldspar having both structurally bound H2O and Pb impurities. Amazonite colour is controlled by either 1) an absorption minimum in the beta spectrum between three overlapping bands in the ultraviolet and a broad band at 625 to 643 nm, resulting in a blue colour, 2) a combination in beta of one UV band and a broad band at 720 nm, resulting in a green colour, or 3) both of the above superimposed, resulting in a blue-green colour. -J.A.Z.
| Original language | English |
|---|---|
| Pages (from-to) | 794-804 |
| Number of pages | 11 |
| Journal | American Mineralogist |
| Volume | 70 |
| Issue number | 7-8 |
| State | Published - 1985 |