Siliceous shale | Siliceous shale | Dominated by authigenic quartz | 0.5-4.0 | ≥50 | ≤10 | ≤10 | ≤10 | ≤10 |
Clay-bearing siliceous shale | Dominated by authigenic quartz | 0.5-2.0 | ≥50 | ≤10 | ≤10 | ≤10 | 10-25 |
Feldspar-bearing siliceous shale | Dominated by authigenic quartz | 0.5-2.0 | ≥50 | 10-25 | ≤10 | ≤10 | ≤10 |
Calcite-bearing siliceous shale | Dominated by authigenic quartz | 0.5-4.0 | ≥50 | ≤10 | 10-25 | ≤10 | ≤10 |
Dolomite-bearing siliceous shale | Dominated by authigenic quartz | 0.5-4.0 | ≥50 | ≤10 | ≤10 | 10-25 | ≤10 |
Clayey shale | Siliceous clayey shale | Dominated by terrigenous grain | ≥8 | 25-50 | ≤10 | ≤10 | ≤10 | 25-50 |
Feldspathic clayey shale | Dominated by terrigenous grain | ≥8 | ≤10 | 25-50 | ≤10 | ≤10 | 25-50 |
Calcareous clayey shale | Dominated by terrigenous grain | ≥8 | ≤10 | ≤10 | 25-50 | ≤10 | 25-50 |
Argillaceous siltstone | Argillaceous siltstone | Dominated by terrigenous grains | 20-50 | 25-50 | ≤10 | 25-50 |
Limy mudstone | Limy mudstone | Dominated by micritic calcite | 20-40 | ≤10 | ≤10 | ≥50 | ≤10 | 25-50 |