Abstract
Stepwise multiple regression analyses of the apparent R(SiO) bond lengths were completed for coesite and for the silica polymorphs together with the clathrasils as a function of the variables fs(O), P(pressure), fs(Si), B(O), and B(Si). The analysis of 94 bond-length data recorded for coesite indicates that all five of these variables make a significant contribution to the regression sum of squares with an R2 value of 0.84. A similar analysis of 245 R(SiO) data recorded for silica polymorphs and clathrasils indicate that only three of the variables (B(O), fs(O), and P) make a significant contribution to the regression with an R2 value of 0.90. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 748-754 |
| Number of pages | 7 |
| Journal | American Mineralogist |
| Volume | 75 |
| Issue number | 7-8 |
| State | Published - 1990 |
ASJC Scopus subject areas
- Geophysics
- Geochemistry and Petrology
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