Changes

Jump to navigation Jump to search
m
Line 1: Line 1:  +
{{publication
 +
| image  = exploring-for-oil-and-gas-traps.png
 +
| width  = 120px
 +
| series  = Treatise in Petroleum Geology
 +
| title  = Exploring for Oil and Gas Traps
 +
| part    = Critical elements of the petroleum system
 +
| chapter = Evaluating source rocks
 +
| frompg  = 6-8
 +
| topg    = 6-9
 +
| author  = Carol A. Law
 +
| link    = http://archives.datapages.com/data/specpubs/beaumont/ch06/ch06.htm
 +
| pdf    =
 +
| store  = http://store.aapg.org/detail.aspx?id=545
 +
| isbn    = 0-89181-602-X
 +
}}
 +
 
The amount of organic carbon present in a rock is a determining factor in a rock's ability to generate hydrocarbons.
 
The amount of organic carbon present in a rock is a determining factor in a rock's ability to generate hydrocarbons.
    
==Effect of depositional environment==
 
==Effect of depositional environment==
[[Depositional environment]] controls the amount of organic carbon contained in a rock. [[Source rock]]s are generally associated with areas where high organic productivity is combined with (1) deposition in poorly oxygenated environments ([[anoxic]] to [[dysaerobic]]), (2) upwelling, and (3) rapid sedimentation.<ref name=ch06r3>Chinn, E., W., 1991, The role of organic geochemistry in petroleum exploration: Basin Research Institute Bulletin, Louisiana State University, Baton Rouge, LA, p. 15–23. ''Short paper that summarizes petroleum geochemistry and its analytical techniques.''</ref>, because these processes preserve organic matter.
+
[[Depositional environments|Depositional environment]] controls the amount of organic carbon contained in a rock. [[Source rock]]s are generally associated with areas where high organic productivity is combined with (1) deposition in poorly oxygenated environments ([[anoxic]] to [[dysaerobic]]), (2) upwelling, and (3) rapid sedimentation,<ref name=ch06r3>Chinn, E., W., 1991, The role of organic geochemistry in petroleum exploration: Basin Research Institute Bulletin, Louisiana State University, Baton Rouge, LA, p. 15–23. ''Short paper that summarizes petroleum geochemistry and its analytical techniques.''</ref> because these processes preserve organic matter.
    
==Average TOCs==
 
==Average TOCs==
The table below (from <ref name=ch06r3 />) shows average TOC values for different sedimentary rock types.
+
The table below<ref name=ch06r3 /> shows average TOC values for different sedimentary rock types.
    
{| class = "wikitable"
 
{| class = "wikitable"
 
|-
 
|-
! Rock type
+
! Rock type || TOC value, %
! TOC value, %
   
|-
 
|-
| Average for all shales
+
| Average for all shales || 0.8
| 0.8
   
|-
 
|-
| Average for shale source rocks
+
| Average for shale source rocks || 2.2
| 2.2
   
|-
 
|-
| Average for calcareous shale source rocks
+
| Average for calcareous shale source rocks || 1.8
| 1.8
   
|-
 
|-
| Average for carbonate source rocks
+
| Average for carbonate source rocks || 0.7
| 0.7
   
|-
 
|-
| Average for all source rocks
+
| Average for all source rocks || 1.8
| 1.8
   
|}
 
|}
   Line 42: Line 52:  
{| class = "wikitable"
 
{| class = "wikitable"
 
|-
 
|-
! Generation potential
+
! [[Petroleum generation|Generation]] potential || Wt % TOC, shales || Wt % TOC, carbonates
! Wt % TOC, shales
  −
! Wt % TOC, carbonates
   
|-
 
|-
| Poor
+
| Poor || 0.0-0.5 || 0.0-0.2
| 0.0-0.5
  −
| 0.0-0.2
   
|-
 
|-
| Fair
+
| Fair || 0.5-1.0 || 0.2-0.5
| 0.5-1.0
  −
| 0.2-0.5
   
|-
 
|-
| Good
+
| Good || 1.0-2.0 || 0.5-1.0
| 1.0-2.0
  −
| 0.5-1.0
   
|-
 
|-
| Very Good
+
| Very Good || 2.0-5.0 || 1.0-2.0
| 2.0-5.0
  −
| 1.0-2.0
   
|-
 
|-
| Excellent
+
| Excellent || > 5.0 || > 2.0
| > 5.0
  −
| > 2.0
   
|}
 
|}
   Line 78: Line 76:  
==References==
 
==References==
 
{{reflist}}
 
{{reflist}}
 +
 +
[[Category:Treatise Handbook 3]]

Navigation menu