dc.contributor.author | Banerjee, R. | |
dc.contributor.author | Iyer, S.D. | |
dc.date.accessioned | 2009-05-06T10:47:14Z | |
dc.date.available | 2009-05-06T10:47:14Z | |
dc.date.issued | 1993 | |
dc.identifier.citation | Journal of the Geological Society of India, Vol.42; 579-584p. | |
dc.identifier.uri | http://drs.nio.org/drs/handle/2264/2862 | |
dc.description.abstract | Pillow 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.iso | en | |
dc.publisher | Geological Society of India | |
dc.rights | Copyright [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.subject | sulphide minerals | |
dc.subject | mineral deposits | |
dc.subject | mineralization | |
dc.subject | basalts | |
dc.title | A note on sulphide-oxide mineralisation in Carlsberg Ridge basalts | |
dc.type | Journal Article | |