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Cutinite

From Wikipedia, the free encyclopedia

Cutinite is a liptinite maceral formed from terrestrial plant cuticles, and often found in coal deposits. It is classified as a Type II kerogen.[1][2]

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References

  1. ^ "Unicorns in the Garden of Good and Evil: Part 2 - Coal" by E R Crain, Can Soc Petrol Geol Reservoir, Dec 2010, Vol 37, issue 11, pages 21-26
  2. ^ "Coal Macerals Tutorial". Archived from the original on 2011-07-20. Retrieved 2011-04-01.


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This article related to petrology is a stub. You can help Wikipedia by expanding it.

Cutinite is a coal maceral of Liptinite group of Macerals derived from waxy outer coating of leaves, roots, and stems. Cutinite is Hydrogen rich and it fluoresces under UV light.

Reference: https://web.archive.org/web/20110720044325/http://mccoy.lib.siu.edu/projects/crelling2/atlas/macerals/mactut.html

This page was last edited on 23 August 2022, at 18:17
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