Kerimasi is an extinct carbonatite-nephelinite volcano located in the Gregory rift in northern Tanzania. It is composed of nephelinitic pyroclastic rocks with carbonatite agglomerates and tuffs.
References
- Hay R.L. (1983): Natrocarbonatite tephra of Kerimasi volcano, Tanzania. Geology 11, 599-602.
- Mariano A.N., Roeder P.L. (1983): Kerimasi: a neglected carbonatite volcano. J. Geology 91, 449-455.
- Church A.A. (1996): The petrology of the Kerimasi carbonatite volcano and the carbonatites of Oldoinyo Lengai with a review of other occurrences of extrusive carbonatites. PhD thesis, University of London, 384 pp.
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http://geo.web.ru/conf/alkaline/2009/Zaitsev2.htmMineral List
3 entries listed. 3 valid minerals. 1 type locality (valid mineral).
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