High-resolution solid-state magic-angle sample-spinning nuclear magnetic resonance (NMR) spectroscopy of layer silicates, including clay minerals, indicate the relationships between the NMR parameters and the structures and compositions of the minerals. These relationships are potentially useful in understanding the crystal chemistry of layer silicates and the chemical and structural changes that take place in them during diagenesis and metamorphism.
|Original language||English (US)|
|Number of pages||12|
|State||Published - May 1985|
ASJC Scopus subject areas
- Geochemistry and Petrology