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 |
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Publisher | SCK CEN |
State | Published - Nov 1962 |
Publication series
Name | SCK•CEN Reports |
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Publisher | Studiecentrum voor Kernenergie |
No. | BLG-164 |