Research Article
Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event
Table 2
Initial mineral contents (%) considered in the reactive transport simulations (for reference see Bea et al., [
9]).
| Mineral | Cr | Crw | Sand1 | Lim1 | Sand2 | Sh1 | Dol1 | Ev | Sh2 | Sand3 | Dol2 | Sand4 | Sh3 | Dol3 |
| Calcite | 0 | 0 | 9 | 89 | 9 | 9 | 10 | 4 | 9 | 9 | 10 | 9 | 9 | 10 | Dolomite | 0 | 0 | 1 | 10 | 1 | 1 | 89.99 | 36 | 1 | 1 | 89.99 | 1 | 1 | 89.99 | Halite | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 50 | 0 | 0 | 0 | 0 | 0 | 0 | Anhydrite | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | 0 |
| Pyrite | 0 | 0 | 0.1 | 0 | 0.1 | 2 | 0 | 0 | 2 | 0.1 | 0 | 0.1 | 0 | 0 | Biotite | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Chlorite | 0.7 | 0.7 | 0 | 0 | 0 | 10 | 0 | 0 | 10 | 0 | 0 | 0 | 0 | 0 | Organic matter | 0 | 0 | 0.1 | 1 | 0.1 | 0.4 | 0.1 | 0 | 0.4 | 0.1 | 0.1 | 0.1 | 10 | 0.1 |
| Nonreactive minerals | 95.3 | 90 | 90.0 | 0 | 90 | 90 | 0 | 0 | 90 | 90 | 0 | 90 | 90 | 0 |
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Based on rock composition for Queenston, Georgian Bay, and Blue Mountain Formations reported by Mazurek [ 1]. |