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Table 5
Models for meteorites from the sample of Yomogida & Matsui (1983) and Opeil et al. (2012) with variable iron volume fraction fir.
| Meteorite | Φop | s | α | fir | χ2 |  |
|---|---|---|---|---|---|---|
| Y-74191 | 17.3 | 307. | 36.7 | 0.157 | 1.753 | 0.292 |
| Farmington | 5.5 | 496. | 88.0 | 0.245 | 4.250 | 0.708 |
| Kunashak | 15.1 | 1000 | 11.3 | 0.227 | 1.726 | 0.288 |
| Arapahoe | 3.3 | 543. | 122. | 0.245 | 1.854 | 0.371 |
| MET-78003 | 15.8 | 532. | 7.23 | 0.163 | 1.932 | 0.386 |
| ALH-769 | 26.9 | 865. | 34.7 | 0.118 | 1.779 | 0.356 |
| Bath Furnace 3 | 6.5 | 62.9 | 2.00 | 0.203 | 8.684 | 0.083 |
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