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Electron Microprobe and Mineralogical Study on Cobalt Bearing Sulphide from the Kalyadi Copper Mine, Hassan District, Karnataka


Affiliations
1 Indian Bureau of Mines, G G Palaya, Bangalore-560022, India
2 Department of Metallurgy, Indian Institute of Science, Bangalore-560012, India
3 Australian Indian Resources, SBI Colony,7th Main, 111 Block, Bangalore-560034, India
4 Indian Bureau of Mines, Indira Bhavan, Civil lines, Nagpur-400001, India
     

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Cobalt mineralisation in the Kalyadi copper-Cobalt deposit in the Hassan district, Karnataka, is mostly in sulphidic banded, feldspathic cherty quartzite. Electron microprobe study conducted on sulphide concentrates from this deposit revealed that cobalt up to 3.21 wt% is present exclusively in pyrite grains, whereas it is absent in chalcopyrite and arsenopyrite. From this, it infers that pyrite crystallized first, followed by chalcopyrite and arsenopyrite with most cobalt present in the mineralizing system replacing Fe in the paragenetically early-Formed pyrite,thereby rendering the system deficient in cobalt during later crystallization of chalcopyrite and arsenopyrite.

Keywords

Pyrite, Cobalt, Electron Microprobe Study, Kalyadi, Karnataka.
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  • Electron Microprobe and Mineralogical Study on Cobalt Bearing Sulphide from the Kalyadi Copper Mine, Hassan District, Karnataka

Abstract Views: 191  |  PDF Views: 2

Authors

Jayasree Thomas
Indian Bureau of Mines, G G Palaya, Bangalore-560022, India
M. S. Riyazulla
Indian Bureau of Mines, G G Palaya, Bangalore-560022, India
S. Subramanian
Department of Metallurgy, Indian Institute of Science, Bangalore-560012, India
V. N. Vasudev
Australian Indian Resources, SBI Colony,7th Main, 111 Block, Bangalore-560034, India
C. S. Gundewar
Indian Bureau of Mines, Indira Bhavan, Civil lines, Nagpur-400001, India

Abstract


Cobalt mineralisation in the Kalyadi copper-Cobalt deposit in the Hassan district, Karnataka, is mostly in sulphidic banded, feldspathic cherty quartzite. Electron microprobe study conducted on sulphide concentrates from this deposit revealed that cobalt up to 3.21 wt% is present exclusively in pyrite grains, whereas it is absent in chalcopyrite and arsenopyrite. From this, it infers that pyrite crystallized first, followed by chalcopyrite and arsenopyrite with most cobalt present in the mineralizing system replacing Fe in the paragenetically early-Formed pyrite,thereby rendering the system deficient in cobalt during later crystallization of chalcopyrite and arsenopyrite.

Keywords


Pyrite, Cobalt, Electron Microprobe Study, Kalyadi, Karnataka.