Difference between revisions of "Type II kerogen"
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(Created page with "File:VanKrevelanDiagram.png|thumb|300px|Van Krevelen diagram.<ref>Dembicki, H., 2009, [http://archives.datapages.com/data/bulletns/2009/03mar/BLTN08076/BLTN08076.HTM Three c...") |
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| + | ==See also== | ||
| + | * [[Kerogen]] | ||
| + | * [[Type I kerogen]] | ||
| + | * [[Type IIS kerogen]] | ||
| + | * [[Type III kerogen]] | ||
| + | * [[Type IV kerogen]] | ||
==References== | ==References== | ||
{{reflist}} | {{reflist}} | ||
Latest revision as of 21:10, 6 July 2015
Van Krevelen diagram.[1]
Oil-prone organic matter having Rock-Eval pyrolysis hydrogen indices in the range of 300 to 600 mg hydrocarbon\g TOC when thermally immature; contains algal and bacterial organic matter dominated by liptinite macerals, such as exinite and sporinite; common but not restricted to marine settings; Type II pathway on Van Krevelen diagrams.[2]
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See also
References
- ↑ Dembicki, H., 2009, Three common source rock evaluation errors made by geologists during prospect or play appraisals: AAPG Bulletin, vol. 93, issue 3, pp. 341-356.
- ↑ Peters, Kenneth E., David J. Curry, and Marek Kacewicz, 2012, An overview of basin and petroleum system modeling: Definitions and concepts, in Peters, Kenneth E., David J. Curry, and Marek Kacewicz, eds., Basin modeling: New horizons in research and applications: AAPG Hedberg Series no. 4, p. 1-16.