Ore-forming processes in the Khetri Copper Belt, western India: constraints from trace element chemistry of pyrite and C-O isotope composition of carbonates

Author(s):  
Abu Saeed Baidya ◽  
Atlanta Sen ◽  
Dipak C. Pal ◽  
Dewashish Upadhyay
2018 ◽  
Author(s):  
Casey Beaudoin ◽  
◽  
G. Nelson Eby

1980 ◽  
Vol 43 (330) ◽  
pp. 765-770 ◽  
Author(s):  
A. M. Duncan ◽  
R. M. F. Preston

SummaryThe chemical variation of clinopyroxene phenocrysts from the trachybasaltic lavas of Etna volcano is described. The phenocrysts show a limited, but distinct trend in chemical variation from calcic-augite in the hawaiites to augite in the benmoreites. The trend of this variation is unusual, being one of Mg-enrichment with differentiation of the magma. Ca shows a steady decrease in the clinopyroxenes from the hawaiites to the benmoreites. Na, however, shows little chemical variation in the pyroxenes. The trace element chemistry is briefly examined. The clinopyroxenes show well-developed oscillatory and sector zoning. The basal {11} sectors are enriched in Si and Mg and depleted in Ti, Al, and Fe relative to the {100}, {110}, and {010} prism sectors.


1994 ◽  
Vol 62 (1-4) ◽  
pp. 429-452 ◽  
Author(s):  
Christopher J. Nye ◽  
Samuel E. Swanson ◽  
Victoria F. Avery ◽  
Thomas P. Miller

1997 ◽  
Vol 29 (1-2) ◽  
pp. 132-141 ◽  
Author(s):  
K. O. Konhauser ◽  
M. A. Powell ◽  
W. S. Fyfe ◽  
F. J. Longstaffe ◽  
S. Tripathy

Minerals ◽  
2013 ◽  
Vol 3 (2) ◽  
pp. 121-144 ◽  
Author(s):  
Simon Goldmann ◽  
Frank Melcher ◽  
Hans-Eike Gäbler ◽  
Stijn Dewaele ◽  
Friso Clercq ◽  
...  

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