Abstract
The Mössbauer resonance absorption is measured in various silicates containing iron. The observed isomeric shifts are in accordance with the interpretation of Walker. Even for Fe3+ ions, large quadrupole splittings are found. The analysis of the spectrum of tourmaline is similar to that of biotite.
| Original language | English |
|---|---|
| Publisher | SCK CEN |
| State | Published - Nov 1962 |
Publication series
| Name | SCK•CEN Reports |
|---|---|
| Publisher | Studiecentrum voor Kernenergie |
| No. | BLG-164 |