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Dawson, J. B., Smith, J. V., Steele, I. M. (1992) 1966 ash eruption of the carbonatite volcano Oldoinyo Lengai: mineralogy of lapilli and mixing of silicate and carbonate magmas. Mineralogical Magazine, 56 (382) 1-16 doi:10.1180/minmag.1992.056.382.01

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Reference TypeJournal (article/letter/editorial)
Title1966 ash eruption of the carbonatite volcano Oldoinyo Lengai: mineralogy of lapilli and mixing of silicate and carbonate magmas
JournalMineralogical MagazineISSN0026-461X
AuthorsDawson, J. B.Author
Smith, J. V.Author
Steele, I. M.Author
Year1992 (March)Volume56
Issue382
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_56/56-382-1.pdf+
DOIdoi:10.1180/minmag.1992.056.382.01Search in ResearchGate
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Mindat Ref. ID1780Long-form Identifiermindat:1:5:1780:4
GUID0
Full ReferenceDawson, J. B., Smith, J. V., Steele, I. M. (1992) 1966 ash eruption of the carbonatite volcano Oldoinyo Lengai: mineralogy of lapilli and mixing of silicate and carbonate magmas. Mineralogical Magazine, 56 (382) 1-16 doi:10.1180/minmag.1992.056.382.01
Plain TextDawson, J. B., Smith, J. V., Steele, I. M. (1992) 1966 ash eruption of the carbonatite volcano Oldoinyo Lengai: mineralogy of lapilli and mixing of silicate and carbonate magmas. Mineralogical Magazine, 56 (382) 1-16 doi:10.1180/minmag.1992.056.382.01
In(1992, March) Mineralogical Magazine Vol. 56 (382) Mineralogical Society
Abstract/NotesAbstractLapilli from the August 1966 eruption of the carbonatite volcano Oldoinyo Lengai consist of carbonate-cemented aggregates of (i) mono- and poly-mineralic fragments of ijolitic rocks, (ii) single grains and clusters of euhedral nepheline, Ti-andradite, and Ti-magnetite, and (iii) corroded pyroxene and wollastonite grains surrounded by coronas containing combeite, melilite, Ca-silicates (possibly larnite and rankinite), and rounded bodies of submicrometre intergrowths with complex bulk compositions dominated by Na,K,Ca-phosphate-carbonate and alkali-iron-sulphide-carbonate. The (ii,iii) materials, together with abundant Na-carbonate, sylvite and fluorite occurring as cement and shells in the lapilli, are attributed to mixing and incomplete reaction of ijolite and carbonatite magmas during the explosive eruption. The rounded submicrometre intergrowths are interpreted as the quench products of two types of immiscible liquids whose properties should be studied by controlled synthesis.


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