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 rocks 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> 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
   
|}
 
|}
    
==Caveat==
 
==Caveat==
Use the table above only as a guide. TOC average values in the real world are meaningless unless we know how the average was calculated. For example, suppose a potential source rock unit is [[length::100 m]] thick. What was the average calculated from:
+
Use the table above only as a guide. TOC average values in the real world are meaningless unless we know how the average was calculated. For example, suppose a potential [[source rock]] unit is [[length::100 m]] thick. What was the average calculated from:
    
* 1 sample, [[length::1 cm]] thick
 
* 1 sample, [[length::1 cm]] thick
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
   
|}
 
|}
    
==Caveat==
 
==Caveat==
If a sample being analyzed for richness is not in an immature state, then the present-day maturation level of the interval needs to be determined to establish an initial (prematuration) organic carbon value for the interval. The measured TOC value is not indicative of the sample's source potential.
+
If a sample being analyzed for richness is not in an immature state, then the present-day [[maturation]] level of the interval needs to be determined to establish an initial (prematuration) organic carbon value for the interval. The measured TOC value is not indicative of the sample's source potential.
    
==See also==
 
==See also==
 
* [[Source rock richness]]
 
* [[Source rock richness]]
* [[Using pyrolysis to estimate richness]]
+
* [[Rock-Eval pyrolysis]]
* [[Using the LECO method to estimate richness]]
+
* [[LECO method in estimating richness]]
 
* [[Using conventional well logs to estimate richness]]
 
* [[Using conventional well logs to estimate richness]]
    
==References==
 
==References==
 
{{reflist}}
 
{{reflist}}
 +
 +
[[Category:Treatise Handbook 3]]

Navigation menu