Alginite
Alginite is a component of some types of kerogen alongside amorphous organic matter. Alginite consists of organic-walled marine microfossils, distinct from inorganic (silica)-walled microfossils that comprise diatomaceous earth. At least two forms of alignite are distinguishable, "alginite A" (telalginite) and "alginite B" (lamalginite).[1] The "A" form contains morphologically distinguishable microfossils while the "B" form is more amorphous and film-like.
References
- ↑ Macauley, G.; Snowdon, L. R.; Ball, F. D. (1985). "Geochemistry and geological factors governing exploitation of selected Canadian oil shale deposits" 85 (13). Natural Resources Canada. p. 3. ISBN 978-0-660-11905-2.
External links
- Akiko Omura and Koichi Hoyanagi (September 2004). "Relationships Between Composition Of Organic Matter, Depositional Environments, And Sea-Level Changes In Backarc Basins, Central Japan (abstract)" (PDF). Journal of Sedimentary Research 74 (5).
- Simon Coxhell and Barry Fehlberg (May 2000). "Julia Creek Vanadium and Oil Shale Deposit". AIG Journal.