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Lawrence, L. J., Bayliss, P., Tonkin, Paul (1968) An occurrence of todorokite in the deuteric stage of a basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 757-760 doi:10.1180/minmag.1968.036.282.01

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Reference TypeJournal (article/letter/editorial)
TitleAn occurrence of todorokite in the deuteric stage of a basalt
JournalMineralogical Magazine and Journal of the Mineralogical Society
AuthorsLawrence, L. J.Author
Bayliss, P.Author
Tonkin, PaulAuthor
Year1968 (June)Volume36
Issue282
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_36/36-282-757.pdf+
DOIdoi:10.1180/minmag.1968.036.282.01Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID6153Long-form Identifiermindat:1:5:6153:1
GUID0
Full ReferenceLawrence, L. J., Bayliss, P., Tonkin, Paul (1968) An occurrence of todorokite in the deuteric stage of a basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 757-760 doi:10.1180/minmag.1968.036.282.01
Plain TextLawrence, L. J., Bayliss, P., Tonkin, Paul (1968) An occurrence of todorokite in the deuteric stage of a basalt. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (282) 757-760 doi:10.1180/minmag.1968.036.282.01
In(1966) Mineralogical Magazine Vol. 36 (282) Mineralogical Society
Abstract/NotesSummaryAn occurrence of todorokite having a formula is recorded from Ardglen, 150 miles N.N.W. of Sydney, New South Wales. The composition of Ardglen todorokite is somewhat simpler than previously recorded occurrences, most of which were in manganese and manganese—base-metal ore deposits. The simpler composition is explained in terms of its occurrence as a late deuteric mineral associated with manganocalcite and zeolites in an altered Tertiary basalt. The manganese is believed to have been derived from the deuteric alteration of the augite of the basalt.


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