The origin of Al-rich spinel inclusions in leucite from the leucite lamproites of Western Australia.

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dc.contributor.authorJaques, A. L.en
dc.contributor.authorFoley, S. F.en
dc.date.accessioned2026-01-01T14:41:59Z
dc.date.available2026-01-01T14:41:59Z
dc.date.issued1985en
dc.description.abstractAluminous spinels (pleonaste-hercynite) occur as tiny (mostly <20 mu m) inclusions in leucite phenocrysts (and pseudomorphs) in leucite lamproites from the West Kimberley region, Western Australia. Their formation in these peralkaline volcanics is attributed to exsolution under conditions of supersaturation from non-stoichiometric leucites originally incorporating Mg, Al and Fe2+ in solid solution. -J.A.Z.en
dc.description.statusPeer-revieweden
dc.format.extent8en
dc.identifier.issn0003-004Xen
dc.identifier.scopus0022227586en
dc.identifier.urihttps://hdl.handle.net/1885/733801084
dc.language.isoenen
dc.sourceAmerican Mineralogisten
dc.titleThe origin of Al-rich spinel inclusions in leucite from the leucite lamproites of Western Australia.en
dc.typeJournal articleen
dspace.entity.typePublicationen
local.bibliographicCitation.lastpage1150en
local.bibliographicCitation.startpage1143en
local.contributor.affiliationJaques, A. L.; Bureau of Mineral Resources, Canberra, ACTen
local.contributor.affiliationFoley, S. F.; University of Tasmaniaen
local.identifier.citationvolume70en
local.identifier.puree0f63019-e45c-4dc7-8568-db3dd31e3145en
local.identifier.urlhttps://www.scopus.com/pages/publications/0022227586en
local.type.statusPublisheden

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