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Dawson, J. B. (1993) A supposed sövite from Oldoinyo Lengai, Tanzania: result of extreme alteration of alkali carbonatite lava. Mineralogical Magazine, 57 (386) 93-101 doi:10.1180/minmag.1993.057.386.09

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Reference TypeJournal (article/letter/editorial)
TitleA supposed sövite from Oldoinyo Lengai, Tanzania: result of extreme alteration of alkali carbonatite lava
JournalMineralogical MagazineISSN0026-461X
AuthorsDawson, J. B.Author
Year1993 (March)Volume57
Issue386
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_57/57-386-93.pdf+
DOIdoi:10.1180/minmag.1993.057.386.09Search in ResearchGate
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Mindat Ref. ID1891Long-form Identifiermindat:1:5:1891:7
GUID0
Full ReferenceDawson, J. B. (1993) A supposed sövite from Oldoinyo Lengai, Tanzania: result of extreme alteration of alkali carbonatite lava. Mineralogical Magazine, 57 (386) 93-101 doi:10.1180/minmag.1993.057.386.09
Plain TextDawson, J. B. (1993) A supposed sövite from Oldoinyo Lengai, Tanzania: result of extreme alteration of alkali carbonatite lava. Mineralogical Magazine, 57 (386) 93-101 doi:10.1180/minmag.1993.057.386.09
In(1993, March) Mineralogical Magazine Vol. 57 (386) Mineralogical Society
Abstract/NotesAbstractA calcite-rich block in nephelinitic agglomerate at Oldoinyo Lengai comprises Sr-calcite, apatite, fluorite, a Ba-Mn oxide akin to romanrchite, and a distinctive Mn-Fe spinel. Formerly reported as sövite, on textural, mineralogical and stable isotope grounds it is now re-interpreted as a highly-altered natrocarbonatite lava. An implication of this study is that natrocarbonatite is not just a modern phenomenon, but has been extruded from Oldoinyo Lengai for at least around 1250 years.


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