Difference between revisions of "Maturation"
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| part = Critical elements of the petroleum system | | part = Critical elements of the petroleum system | ||
| chapter = Evaluating source rocks | | chapter = Evaluating source rocks | ||
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| − | | topg = 6- | + | | topg = 6-22 |
| author = Carol A. Law | | author = Carol A. Law | ||
| link = http://archives.datapages.com/data/specpubs/beaumont/ch06/ch06.htm | | link = http://archives.datapages.com/data/specpubs/beaumont/ch06/ch06.htm | ||
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| − | The chemistry of organic matter contained within a sedimentary rock changes over time, reflecting its [[Thermal history|thermal]] 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]], | + | The chemistry of organic matter contained within a sedimentary rock changes over time, reflecting its [[Thermal history|thermal]] 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, [[Wikipedia:Fluid dynamics|fluid flow]], rock matrix chemistry, and [[Petroleum reservoir fluid properties|pore fluid chemistry]] can affect the thermal history and thus a rock's rate of maturation. |
==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, [[spore]]s, [[apatite]] grains, and [[biomarker]]s; 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 [[Kerogen types: comparison of maturity measures|maturity levels]] and (2) have different transformation rates. Maturity measurements can be made on several different components of a rock like [[Thermal maturation#Vitrinite|vitrinite]], [[kerogen]], [[spore]]s, [[apatite]] grains, and [[biomarker]]s; each has its own relationship to the kerogen transformation rate. |
==Caveat== | ==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. | 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|T<sub>max</sub>]] 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. | + | For example, [[Tmax|T<sub>max</sub>]] cutoffs for [[Petroleum generation|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== | ==See also== | ||
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* [[Hydrogen Index (HI)]] | * [[Hydrogen Index (HI)]] | ||
* [[Production Index (PI)]] | * [[Production Index (PI)]] | ||
| + | * [[Kerogen type and maturity]] | ||
| + | * [[Kerogen types: comparison of maturity measures]] | ||
==External links== | ==External links== | ||
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[[Category:Critical elements of the petroleum system]] | [[Category:Critical elements of the petroleum system]] | ||
[[Category:Evaluating source rocks]] | [[Category:Evaluating source rocks]] | ||
| + | [[Category:Treatise Handbook 3]] | ||
Latest revision as of 18:26, 9 February 2022
| 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 thermal 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)
- Kerogen type and maturity
- Kerogen types: comparison of maturity measures
External links
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