Line 95: |
Line 95: |
| ===Dunham’s Criteria=== | | ===Dunham’s Criteria=== |
| Dunham classification system is based on three depositional textural features: | | Dunham classification system is based on three depositional textural features: |
− | • The presence or absence of lime mud.
| + | * The presence or absence of lime mud. |
− | • The abundance of grains.[j]
| + | * The abundance of grains.[j] |
− | • the presence of in situ organic binding
| + | * The presence of in situ organic binding |
| | | |
| ===Dunham (1962) Classification=== | | ===Dunham (1962) Classification=== |
| + | [[File:GeoWikiWriteOff2021-Abdulwahab-Figure12.png|thumbnail|400px|{{Figure number|12}}Dunham classification system for carbonate rock (1962)]] |
| The original Dunham classification system composes of six classes summarized in Figure 12: | | The original Dunham classification system composes of six classes summarized in Figure 12: |
− | [[File:GeoWikiWriteOff2021-Abdulwahab-Figure12.png|thumbnail|Fig. 12 Dunham classification system for carbonate rock (1962) [12]]] | + | * [[Mudstone]]: a mud-supported rock with < 10% grains, and original components are not organically bounded together during deposition (Figure 13). |
− | | + | * Wackestone: a mud-supported rock with > 10% grains, and original components are not organically bounded together during deposition (Figure 14). |
− | • Mudstone: a mud-supported rock with < 10% grains, and original components are not organically bounded together during deposition (Figure 13).
| + | * Packstone: a grain-supported rock with lime mud presented, and original components are not organically bounded together during deposition (Figure 15). |
− | • Wackestone: a mud-supported rock with > 10% grains, and original components are not organically bounded together during deposition (Figure 14).
| + | * Grainstone: a grain-supported rock with lime mud absent, and original components are not organically bounded together during deposition (Figure 16). |
− | • Packstone: a grain-supported rock with lime mud presented, and original components are not organically bounded together during deposition (Figure 15).
| + | * Boundstone: a rock with the presence of organic components bounded together during deposition. |
− | • Grainstone: a grain-supported rock with lime mud absent, and original components are not organically bounded together during deposition (Figure 16).
| + | * Crystalline: a rock with unrecognizable depositional texture (Figure 17). |
− | • Boundstone: a rock with the presence of organic components bounded together during deposition.
| |
− | • Crystalline: a rock with unrecognizable depositional texture (Figure 17).
| |
| | | |
| ===Extended Dunham Classification (1971)=== | | ===Extended Dunham Classification (1971)=== |
Line 130: |
Line 129: |
| Floatstones and bindstones are usually formed in medium-energy settings (below average wave base). | | Floatstones and bindstones are usually formed in medium-energy settings (below average wave base). |
| Rudstones and framestones are usually formed in high-energy settings (above wave base). | | Rudstones and framestones are usually formed in high-energy settings (above wave base). |
− | Organically-bound rocks show good reservoir quality if the skeletal growth is interconnected. | + | Organically-bound rocks show good reservoir quality if the skeletal growth is interconnected. |
| | | |
| ==Gallery== | | ==Gallery== |