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| {| class = "wikitable" | | {| class = "wikitable" |
| |- | | |- |
− | ! Zone | + | ! rowspan = 2 | Zone || rowspan = 2 | Temperature || colspan = 2 | Major diagenetic processes |
− | ! Temp.
| |
− | ! Major diagenetic processes
| |
− | ! Preserves or enhances porosity
| |
− | ! Destroys porosity
| |
| |- | | |- |
− | | Shallow | + | ! Preserves or enhances porosity || Destroys porosity |
− | |
| |
− | | |
− | | * Grain coatings (inhibit later overgrowths) * Nonpervasive carbonate cements that can be dissolved later
| |
− | | |
− | | * Clay infiltration * Carbonate or silica cement (in some cases irreversible) * Authigenic kaolinite * Compaction of [[Ductility|ductile]] grains
| |
− | | |
| |- | | |- |
− | | Intermediate | + | | Shallow || <80°C or 176°F (<5,00 to 10,00 ft) |
− | | [[temperature::80-140°C]] or 176–[[temperature::284°F]] | + | | |
− | | * Carbonate cement dissolved * Feldspar grains dissolved | + | * Grain coatings (inhibit later overgrowths) |
− | | + | * Nonpervasive carbonate cements that can be dissolved later |
− | | * Kaolinite, chlorite, and illite precipitate as a result of feldspar dissolution * Ferroan carbonate and quartz cement
| + | | |
− | | + | * Clay infiltration |
| + | * Carbonate or silica cement (in some cases irreversible) |
| + | * Authigenic kaolinite |
| + | * Compaction of [[Ductility|ductile]] grains |
| + | |- |
| + | | Intermediate || 80-140°C or 176–284°F |
| + | | |
| + | * Carbonate cement dissolved |
| + | * Feldspar grains dissolved |
| + | | |
| + | * Kaolinite, chlorite, and illite precipitate as a result of feldspar dissolution |
| + | * Ferroan carbonate and quartz cement |
| |- | | |- |
| | Deep | | | Deep |
− | | > [[temperature::140°C]] or [[temperature::284°F]] | + | | > 140°C or 284°F |
− | | * Feldspar, carbonate, and sulfate minerals dissolved | + | | |
− | | + | * Feldspar, carbonate, and sulfate minerals dissolved |
− | | * Quartz cement (most destructive) * Kaolinite precipitation * Illite, chlorite form as products of feldspar dissolution * Pyrite precipitation | + | |- |
− | | + | | |
| + | * Quartz cement (most destructive) |
| + | * Kaolinite precipitation |
| + | * Illite, chlorite form as products of feldspar dissolution |
| + | * Pyrite precipitation |
| |} | | |} |
| | | |