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Scott Smith, Barbara H., Michael Skinner, E., Roger Clement, C. (1983) Further data on the occurrence of pectolite in kimberlite. Mineralogical Magazine, 47 (342) 75-78 doi:10.1180/minmag.1983.047.342.13

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Reference TypeJournal (article/letter/editorial)
TitleFurther data on the occurrence of pectolite in kimberlite
JournalMineralogical MagazineISSN0026-461X
AuthorsScott Smith, Barbara H.Author
Michael Skinner, E.Author
Roger Clement, C.Author
Year1983 (March)Volume47
Issue342
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_47/47-342-75.pdf+
DOIdoi:10.1180/minmag.1983.047.342.13Search in ResearchGate
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Mindat Ref. ID3475Long-form Identifiermindat:1:5:3475:7
GUID0
Full ReferenceScott Smith, Barbara H., Michael Skinner, E., Roger Clement, C. (1983) Further data on the occurrence of pectolite in kimberlite. Mineralogical Magazine, 47 (342) 75-78 doi:10.1180/minmag.1983.047.342.13
Plain TextScott Smith, Barbara H., Michael Skinner, E., Roger Clement, C. (1983) Further data on the occurrence of pectolite in kimberlite. Mineralogical Magazine, 47 (342) 75-78 doi:10.1180/minmag.1983.047.342.13
In(1983, March) Mineralogical Magazine Vol. 47 (342) Mineralogical Society
Abstract/NotesAbstractPectolite has been identified, using petrographic, chemical, and X-ray methods, in kimberlites from the De Beers and Dutoitspan Mines, Kimberley, South Africa and the Letseng-La-Terai Mine, Lesotho. It occurs as radiating aggregates of fibrous or acicular crystals not only in the groundmass of certain kimberlites but also in altered xenoliths included within kimberlite. The occurrence of Na-rich minerals in kimberlite is unusual. It is suggested that it can occur as an apparently primary mineral resulting from the incorporation and assimilation of foreign Na-bearing material prior to final consolidation, and/or as a secondary mineral after metasomatic introduction of Na-bearing fluids.

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