Table 4
Result of mass balance calculations, calculated with the statistical Isocon method of Baumgartner and Olsen (1995), between the ‘altered’ schists in shear zones and the ‘host’ metagabbros.
| value | 1σ | value (%) | 1σ (%) | |
|---|---|---|---|---|
| M0/MA | 0.50 | 0.04 | ||
| χ2 | 1.36 | |||
| χ2 / (n-1) | 0.45 | |||
| Q | 0.51 | |||
| ni / 11 | 4.00 | |||
| Mass change | 1.02 | 0.16 | 101.59 | 16.37 |
| Dens. change | -0.04 | 0.00 | -4.39 | 0.35 |
| Vol. change | 1.11 | 0.61 | 110.85 | 61.44 |
| Mass change (g.100g-1) | ||||
| SiO2 | 42.96 | 8.33 | 88 | 17 |
| Al2O3 | -0.71 | 2.15 | -4 | 12 |
| Fe2O3 | 9.11 | 2.42 | 214 | 57 |
| MnO | 0.12 | 0.03 | 135 | 31 |
| MgO | 43.15 | 5.71 | 399 | 53 |
| CaO | 0.32 | 2.39 | 2 | 18 |
| Na2O | -1.94 | 0.41 | -83 | 17 |
| K2O | 0.05 | 0.03 | 71 | 44 |
| TiO2 | 0.08 | 0.08 | 38 | 38 |
| P2O5 | 0 | 0.02 | 12 | 69 |
| L.O.I. | 8.46 | 2.19 | 270 | 70 |
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