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A note on sulphide-oxide mineralisation in Carlsberg Ridge basalts

IR@NIO: CSIR-National Institute Of Oceanography, Goa

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Field Value
 
Creator Banerjee, R.
Iyer, S.D.
 
Date 2009-05-06T10:47:14Z
2009-05-06T10:47:14Z
1993
 
Identifier Journal of the Geological Society of India, Vol.42; 579-584p.
http://hdl.handle.net/2264/2862
 
Description 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
 
Language en
 
Publisher Geological Society of India
 
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.
 
Subject sulphide minerals
mineral deposits
mineralization
basalts
 
Title A note on sulphide-oxide mineralisation in Carlsberg Ridge basalts
 
Type Journal Article