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

Based on rock composition for Queenston, Georgian Bay, and Blue Mountain Formations reported by Mazurek [1].