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! Characteristics
 
! Characteristics
 
|-
 
|-
| Sandstones
+
| colspan = 2 | Sandstones
|
      
|-
 
|-
|   Primary intergranular
+
| Primary intergranular
 
| Interstitial void space between framework grains
 
| Interstitial void space between framework grains
 
|-
 
|-
|   Dissolution or vug
+
| Dissolution or vug
 
| Partial or complete dissolution of framework grains or cement
 
| Partial or complete dissolution of framework grains or cement
 
|-
 
|-
|   Micropores
+
| Micropores
 
| Small pores mainly between detrital or authigenic clays; can also occur within grains (e.g., microporous chert)
 
| Small pores mainly between detrital or authigenic clays; can also occur within grains (e.g., microporous chert)
 
|-
 
|-
|   Fracture
+
| Fracture
 
| Breakage due to earth stresses
 
| Breakage due to earth stresses
 
|-
 
|-
| Carbonates
+
| colspan = 2 | Carbonates
|
      
|-
 
|-
|   Interparticle
+
| Interparticle
 
| Pores between particles or grains
 
| Pores between particles or grains
 
|-
 
|-
|   Intraparticle
+
| Intraparticle
 
| Pores within individual particles or grains
 
| Pores within individual particles or grains
 
|-
 
|-
|   Intercrystal
+
| Intercrystal
 
| Pores between crystals
 
| Pores between crystals
 
|-
 
|-
|   Moldic
+
| Moldic
 
| Pores formed by dissolution of an individual grain or crystal in the rock
 
| Pores formed by dissolution of an individual grain or crystal in the rock
 
|-
 
|-
|   Fenestral
+
| Fenestral
 
| Primary pores larger than grain-supported interstices
 
| Primary pores larger than grain-supported interstices
 
|-
 
|-
|   Fracture
+
| Fracture
 
| Formed by a planar break in the rock
 
| Formed by a planar break in the rock
 
|-
 
|-
|   Vug
+
| Vug
 
| Large pores formed by indiscriminate dissolution of cements and grains
 
| Large pores formed by indiscriminate dissolution of cements and grains
 
|}
 
|}

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