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Nawaz, Rab, Ryback, George (1989) Re-examination of kirwanite: a ferri-ferro-hornblende from Co. Down, Northern Ireland. Mineralogical Magazine, 53 (370) 253-255 doi:10.1180/minmag.1989.053.370.13

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Reference TypeJournal (article/letter/editorial)
TitleRe-examination of kirwanite: a ferri-ferro-hornblende from Co. Down, Northern Ireland
JournalMineralogical MagazineISSN0026-461X
AuthorsNawaz, RabAuthor
Ryback, GeorgeAuthor
Year1989 (April)Volume53
Issue370
PublisherMineralogical Society
Download URLhttps://rruff.info/doclib/MinMag/Volume_53/53-370-253.pdf+
DOIdoi:10.1180/minmag.1989.053.370.13Search in ResearchGate
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Mindat Ref. ID1499Long-form Identifiermindat:1:5:1499:5
GUID0
Full ReferenceNawaz, Rab, Ryback, George (1989) Re-examination of kirwanite: a ferri-ferro-hornblende from Co. Down, Northern Ireland. Mineralogical Magazine, 53 (370) 253-255 doi:10.1180/minmag.1989.053.370.13
Plain TextNawaz, Rab, Ryback, George (1989) Re-examination of kirwanite: a ferri-ferro-hornblende from Co. Down, Northern Ireland. Mineralogical Magazine, 53 (370) 253-255 doi:10.1180/minmag.1989.053.370.13
In(1989, April) Mineralogical Magazine Vol. 53 (370) Mineralogical Society
Abstract/NotesAbstractX-ray powder, optical, infrared, and chemical data suggest that kirwanite is an amphibole of composition (Na,K)0.10Ca1.80(Fe2+,Mn)3.10Mg0.79Fe1.143+Al0.78Si7.18O22(OH)2 and thus corresponds to ferri-ferro-hornblende (Leake, 1978). The type locality, originally given as the NE coast of Ireland, is most likely Dunmore Head, Co. Down. Kirwanite occurs in the groundmass and the vesicles of variolitic andesite dykes of the Mourne dyke swarm. Thomson's original analysis of kirwanite was probably made on a mixture and the name should not be used for an amphibole species.

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