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Clarke, M. G. C., Roberts, B. (1986) Carbonated melilitites and calcitized alkalicarbonatites from Homa Mountain, western Kenya: a reinterpretation. Geological Magazine, 123 (6) 683-692 doi:10.1017/s0016756800024195

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Reference TypeJournal (article/letter/editorial)
TitleCarbonated melilitites and calcitized alkalicarbonatites from Homa Mountain, western Kenya: a reinterpretation
JournalGeological Magazine
AuthorsClarke, M. G. C.Author
Roberts, B.Author
Year1986 (November)Volume123
Page(s)683-692Issue6
PublisherCambridge University Press (CUP)
DOIdoi:10.1017/s0016756800024195Search in ResearchGate
Mindat Ref. ID253295Long-form Identifiermindat:1:5:253295:4
GUID53da947c-bf40-4f11-a865-c1945bec1f4e
Full ReferenceClarke, M. G. C., Roberts, B. (1986) Carbonated melilitites and calcitized alkalicarbonatites from Homa Mountain, western Kenya: a reinterpretation. Geological Magazine, 123 (6) 683-692 doi:10.1017/s0016756800024195
Plain TextClarke, M. G. C., Roberts, B. (1986) Carbonated melilitites and calcitized alkalicarbonatites from Homa Mountain, western Kenya: a reinterpretation. Geological Magazine, 123 (6) 683-692 doi:10.1017/s0016756800024195
In(1986, November) Geological Magazine Vol. 123 (6) Cambridge University Press (CUP)
Abstract/NotesAbstractHoma Mountain is a well developed ijolite/carbonatite complex of Miocene to Quaternary age. Late stage olivine melilitite occurs as a satellite plug, parts of which show strong deuteric alteration to carbonate resulting in complete pseudomorphing of the melilite.A second satellite centre exposes a grey carbonate tuff and accompanying dykes, all of which exhibit relic textures after an elongate, rectangular mineral also formerly believed to be melilite. Comparison with other recently described occurrences indicates however that the second centre erupted alkali-carbonatite and that the chief mineral originally present was nyerereite (Na2Ca(CO3)2). The field relationships and petrographic characters of both rock types are described and criteria are given which permit distinction between carbonated melilite and calcitized nyerereite. It is concluded that olivine melilitite and alkalicarbonatite are closely related in space and time.

References Listed

These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.

Nurse (1953) Journal of the Iron and Steel Institute Studies in the melilite solid solutions 174, 121
Flegg (1977) Carbonatite–Nephelinite Volcanism: An African Case History
Clarke (1979) Carbonatite–Nephelinite Volcanism: An African Case History , 208
Le Bas (1977) Carbonatite–Nephelinite Volcanism: An African Case History
Saggerson. (1952) Geological Survey of Kenya, report Geology of the Kisumu District
Dixon (1977) Carbonatite–Nephelinite Volcanism: An African Case History , 169


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