Difference between revisions of "Maturation"
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==Transformation rate== | ==Transformation rate== | ||
| − | The rate at which hydrocarbons are generated from organic matter is called the transformation rate. Using source rock maturity, we can estimate the transformation rate. Different kerogen types (1) generate hydrocarbons at different maturity levels and (2) have different transformation rates. Maturity measurements can be made on several different components of a rock like vitrinite, kerogen, spores, apatite grains, and biomarkers; each has its own relationship to the kerogen transformation rate. | + | The rate at which hydrocarbons are generated from organic matter is called the transformation rate. Using source rock maturity, we can estimate the transformation rate. Different [[kerogen types]] (1) generate hydrocarbons at different maturity levels and (2) have different transformation rates. Maturity measurements can be made on several different components of a rock like vitrinite, kerogen, spores, apatite grains, and biomarkers; each has its own relationship to the kerogen transformation rate. |
==Caveat== | ==Caveat== | ||
Revision as of 19:56, 26 February 2014
| Exploring for Oil and Gas Traps | |
| |
| Series | Treatise in Petroleum Geology |
|---|---|
| Part | Critical elements of the petroleum system |
| Chapter | Evaluating source rocks |
| Author | Carol A. Law |
| Link | Web page |
| Store | AAPG Store |
The chemistry of organic matter contained within a sedimentary rock changes over time, reflecting its temperature and burial history. This change or maturation is measured and can be combined with quality and richness data to gauge the amount of hydrocarbon generated by the organic matter. The present-day maturity level is the product of a number of variables, such as tectonic setting, burial history, and thermal history. A number of variables such as paleolatitude, pressure, fluid flow, rock matrix chemistry, and pore fluid chemistry can affect the thermal history and thus a rock's rate of maturation.
Transformation rate
The rate at which hydrocarbons are generated from organic matter is called the transformation rate. Using source rock maturity, we can estimate the transformation rate. Different kerogen types (1) generate hydrocarbons at different maturity levels and (2) have different transformation rates. Maturity measurements can be made on several different components of a rock like vitrinite, kerogen, spores, apatite grains, and biomarkers; each has its own relationship to the kerogen transformation rate.
Caveat
Evaluating the maturation of a geologic section is based on a depth trend from samples in a well or basin. The level of maturity interpreted from most maturation indices is dependent on the type of organic matter or material being analyzed.
For example, Tmax cutoffs for hydrocarbon-generation zones are greater for type III than for type II kerogen. Therefore, a trend is only valid if based on analysis of samples from a homogeneous organic sequence or if differences in chemistry are accounted for in the interpretation process.
See also
- Evaluating source rock maturity
- Tmax
- Vitrinite reflectance
- Apatite fission track analysis
- Spore coloration and thermal alteration indices
- Hydrogen Index (HI)
- Production Index (PI)
External links
| find literature about Maturation |
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