The 353 Ga St James Volcanogenic Massive Sulfide Deposit Kaapvaal Craton Links to Submarine Rhyolites Not to Komatiites

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dc.article.end-page924en
dc.article.start-page903en
dc.citation.doi10.5382/ECONGEO.5162en
dc.contributor.authorT Netshidzivheen
dc.contributor.authorS Tappeen
dc.contributor.authorAllan Wilsonen
dc.contributor.authorS Burnessen
dc.contributor.authorKathleen Smarten
dc.contributor.authoret alen
dc.date.accessioned2025-10-21T11:13:56Z
dc.facultyFACULTY OF SCIENCEen
dc.identifier.citationWOSen
dc.identifier.issn0361-0128en
dc.identifier.urihttps://hdl.handle.net/10539/47152
dc.journal.titleThe 353 Ga St James Volcanogenic Massive Sulfide Deposit Kaapvaal Craton Links to Submarine Rhyolites Not to Komatiitesen
dc.journal.volume120en
dc.titleThe 353 Ga St James Volcanogenic Massive Sulfide Deposit Kaapvaal Craton Links to Submarine Rhyolites Not to Komatiitesen
dc.typeJournal Articleen

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