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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&deg;C or 176&deg;F (<5,00 to 10,00 ft)
| [[temperature::80-140&deg;C]] or 176–[[temperature::284&deg;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&deg;C or 176–284&deg;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&deg;C]] or [[temperature::284&deg;F]]
+
| > 140&deg;C or 284&deg;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
 
|}
 
|}
  

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