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Dawson, J. B. (1997) Neogene–Recent rifting and volcanism in northern Tanzania: relevance for comparisons between the Gardar province and the East African Rift valley. Mineralogical Magazine, 61 (407) 543-548 doi:10.1180/minmag.1997.061.407.06

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Reference TypeJournal (article/letter/editorial)
TitleNeogene–Recent rifting and volcanism in northern Tanzania: relevance for comparisons between the Gardar province and the East African Rift valley
JournalMineralogical MagazineISSN0026-461X
AuthorsDawson, J. B.Author
Year1997 (August)Volume61
Issue407
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_61/61-407-543.pdf+
DOIdoi:10.1180/minmag.1997.061.407.06Search in ResearchGate
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Mindat Ref. ID192Long-form Identifiermindat:1:5:192:4
GUID0
Full ReferenceDawson, J. B. (1997) Neogene–Recent rifting and volcanism in northern Tanzania: relevance for comparisons between the Gardar province and the East African Rift valley. Mineralogical Magazine, 61 (407) 543-548 doi:10.1180/minmag.1997.061.407.06
Plain TextDawson, J. B. (1997) Neogene–Recent rifting and volcanism in northern Tanzania: relevance for comparisons between the Gardar province and the East African Rift valley. Mineralogical Magazine, 61 (407) 543-548 doi:10.1180/minmag.1997.061.407.06
In(1997, August) Mineralogical Magazine Vol. 61 (407) Mineralogical Society
Abstract/NotesAbstractThe tectonic position of the intraplate, alkaline volcanic province of N. Tanzania in a broad rift-controlled area astride the boundary between the Tanzania Craton and the circum-cratonic Mozambique Fold Belt, strongly resembles that of the Gardar province of S. Greenland. Earlier-identified petrological analogies between Gardar magmatism and that in the Kenya sector of the East African Rift Valley can be extended to volcanism in N. Tanzania, and analogies specifically with the Gardar agpaitic suite are strengthened by the occurrence of eudialyte and aenigmatite in some Tanzanian peralkaline, silicic volcanics.


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