Source rocks are subsurface sedimentary rock usually shale or limestone, they have the ability of generating or already generated movable quantities of hydrocarbons.
A rock should have following features to be a source rock:
1.Organic matter availability in sufficient amount
2.Should be able to produce movable hydrocarbons
3.Thermal maturity.
Source rocks are mainly categorized into three basic categories on the basis of kerogen they contain. They are described in the next table
Source rock potential is determined using below table:-
Measuring the “Total organic carbon “(TOC) present in weight percent (wt %) is the most common method for determining source rock potential. Hydrocarbons are 75-95 wt % carbon by molecular weight and average 83 wt %. The organic carbon quantity present in rock determines rock’s ability to generate hydrocarbons. In below table (from Chinn,E.W ,1991) we are presenting average total organic carbon (TOC) values for various sedimentary rock .
Rock type | TOC ( %) |
“Shale averages” | 0.8 |
“Shale source rock averages” | 2.2 |
“Calcareous shale source rock averages” | 1.8 |
“Carbonate source rock averages” | 0.7 |
“All source rock averages” | 1.8 |
In the below table assessment guidelines to estimate source rock richness is presented
Generation Potential | Shales TOC in Wt % | Carbonates TOC in Wt % |
Poor | 0.0 to0.5 | 0.0 to0.2 |
Fair | 0.5 to1.0 | 0.2 to0.5 |
Good | 1.0 to2.0 | 0.5 to1.0 |
Very Good | 2.0 to5.0 | 1.0 to2.0 |
Excellent | Greater than 5.0 | Greater than 2.0 |
If the analyzed sample to find out sample richness is mature , then the current maturity is determined to find the initial (pre-maturation) value of organic carbon for the given interval. The TOC value found does not help in identifying source potential of sample
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