Research Article
Evaluation of the Potential for Dissolved Oxygen Ingress into Deep Sedimentary Basins during a Glaciation Event
Figure 2
Initial distribution of the volumetric contents of redox-buffering minerals. (a), (b), (c), and (d) are pyrite, organic matter, biotite, and chlorite contents, respectively. Vertical exaggeration 100 : 1.
(a) Pyrite |
(b) Solid Organic Matter (SOM) |
(c) Biotite |
(d) Chlorite |