Abstract
Coordination of sulfur is determined by comparing the wavelengths of sulfur K! radiation produced by fluorescent excitation of calcium sulfide, calcium sulfite and calcium sulfate (gypsum), with the wavelengths of the fluorescent radiation emitted by two samples of sulfur-rich scapolite, one from Laacher See in Germany and the other from Delegat, Australia.
| Original language | English |
|---|---|
| Pages (from-to) | 1735-1738 |
| Number of pages | 4 |
| Journal | American Mineralogist |
| Volume | 53 |
| Issue number | 9-10 |
| Publication status | Published - Sept 1968 |