Difference between revisions of "Type III kerogen"
Jump to navigation
Jump to search
(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...") |
m (added Category:Stubs using HotCat) |
||
| Line 9: | Line 9: | ||
==References== | ==References== | ||
{{reflist}} | {{reflist}} | ||
| + | |||
| + | [[Category:Stubs]] | ||
Revision as of 20:54, 6 July 2015
Van Krevelen diagram.[1]
Gas-prone organic matter having Rock-Eval pyrolysis hydrogen indices in the range of 50 to 200 mg hydrocarbon\g TOC when thermally immature; generally contains higher plant organic matter dominated by vitrinite macerals; common but not restricted to paralic marine settings; type III pathway on Van Krevelen diagrams.[2]
This article is a stub. You can help AAPG Wiki by expanding it.
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.