Abstract
The atomic displacement parameters (ADPs) obtained from published refinements of silicate crystals measured at or below room temperature are examined to determine if TO4 (T = Al,Si) tetrahedra display rigid-body thermal motion. In many cases, the correlation found among the ADPs is consistent with the TLS model of rigid-body motion. The libration angle for rigid tetrahedra is quadratically dependent on the difference between the isotropic equivalent displacement parameter of the T and O atoms, Beq(T) and Beq(O), respectively. The value of Beq(O) is on average twice that of Beq(T), with an observed maximum value of ~2.0 Å3. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 680-690 |
| Number of pages | 11 |
| Journal | American Mineralogist |
| Volume | 80 |
| Issue number | 7-8 |
| DOIs | |
| State | Published - 1995 |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
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