Oil & Gas
- comes from organic matter (OM) through transformation involving heat and geologic time
Source Rocks
- capable of generating oil & gas
- must be:
* rich in organic content
* mature enough to expel the oil or gas
Organic Matter
- material composed of organic molecules
- all organic matter was originally atmospheric CO2
3.1 -3.3 BYA - oldest form of organic life
3.7 - 4 BYA - oldest know rocks
Pre-Cambrian to Devonian - marine phytoplankton
Devonian - increasing amount from terrestrial sources
4 Contributors of OM
1. Phytoplankton
2. Zooplanktons
3. Higher plants
4. Bacteria
Sequence of OM
- Production
- Accumulation
- Preservation
Production of OM
- controlled by LIGHT, TEMPERATURE & CHEMICAL COMPOSITION of sea water
- 60 to 80 meters (large part of biological production)
- coastal waters 2x as that of open seas productivity
Accumulation & Preservation of OM
- restricted to an aquatic environment
- to high energy level causes erosion & high sed rate
- to low, little sed supplied to bury the OM
- anoxic environment
- fine-grained more favorable
- continental shelf: lagoons, estuaries and deep basins
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