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dc.contributor.authorBanerjee, R.
dc.contributor.authorIyer, S.D.
dc.date.accessioned2009-05-06T10:47:14Z
dc.date.available2009-05-06T10:47:14Z
dc.date.issued1993
dc.identifier.citationJournal of the Geological Society of India, Vol.42; 579-584p.
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/2862
dc.description.abstractPillow basalts from the Carlsberg Ridge at 3 degrees 35'N contain disseminated chalcopyrite, pyrite, and magnetite. The euhedral shape of the pyrite grains indicate them to be early formed and grown unobstructed while magnetite occurs as skeletal crystals. These opaque minerals indicate their origin from a rapidly cooled silicate melt and probably resultEd. by a process of liquid immiscibility during lava emplacement
dc.language.isoen
dc.publisherGeological Society of India
dc.rightsCopyright [1993]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository.
dc.subjectsulphide minerals
dc.subjectmineral deposits
dc.subjectmineralization
dc.subjectbasalts
dc.titleA note on sulphide-oxide mineralisation in Carlsberg Ridge basalts
dc.typeJournal Article


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