Abstract
The apparent SiO bond lengths recorded for silicates over a range of temperatures either typically are invariant or exhibit a contraction with increasing temperature. A rigid-body thermal analysis was completed for the tetrahedra in nine silicates whose structures have been determined over a range of temperatures from 15 to 1250 K and whose tetrahedra seem to behave as rigid units. The bond lengths and volumes estimated for tetrahedra with four bridging O atoms seem to increase with temperature at a faster rate than those with four nonbridging O atoms. Those for tetrahedra with two or three nonbridging O atoms tend to increase an an intermediate rate. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 751-757 |
| Number of pages | 7 |
| Journal | American Mineralogist |
| Volume | 77 |
| Issue number | 7-8 |
| State | Published - 1992 |
| Externally published | Yes |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology