Geochemical evidence for a Neoproterozoic magmatic continental margin in Sri Lanka relevance for the Rodinia-Gondwana supercontinent cycle

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dc.contributor.authorWillbold, M.
dc.contributor.authorHegner, E.
dc.contributor.authorKleinschrodt, R.
dc.contributor.authorStosch, H.G.
dc.contributor.authorKehelpannala, K.V.W.
dc.contributor.authorDulski, P.
dc.date.accessioned2015-12-30T04:20:50Z
dc.date.available2015-12-30T04:20:50Z
dc.date.issued2004
dc.identifier.citationPrecambrian Research, 130:p.185-198
dc.identifier.urihttps://dl-ifs.nsf.gov.lk/handle/1/961
dc.titleGeochemical evidence for a Neoproterozoic magmatic continental margin in Sri Lanka relevance for the Rodinia-Gondwana supercontinent cycle
dc.typeArticle

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