A note on the bornite-chalcopyrite intergrowth texture in the volcanic-hosted copper mineralization in the Dir area, northern Pakistan

Authors

  • Mohammad Tahir Shah National Centre of Excellence in Geology, University of Peshawar, Pakistan

Abstract

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References

Condit, R. H., Hobbins, R. R. & Birchenall, C. E., 1974. Self-diffusion of iron and sulfur in ferrous sulfide. Oxid., Met., 8, 409-455.

Durazzo, A. & Taylor, A. A., 1982. Experimental ex-solution texture in the system bornitechalcopyrite: genetic implications concerning natural ores. Mineralium Deposita, 17, 79-97.

Lafitte, M., Maury, R. & Perseil, E. A., 1983. Influence de la composition du milien hydrothermal de formation sur la stoichiometrie de chalcopyrites. Comparison avee les mineralsations de dorsales oceaniques. C. R. Acad. Sci. France, I l, 296, 567-570.

Lafitte, M., Maury, R., Perseil, E. A. & Boulegue., 1985. Morphological and analytical study of hydrothermal sulfides from 21 north-east Pacific Rise. Earth Planet. Sci. Lett., 73, 53-64.

Lyon, R. J. P., 1959. Time aspects of geothermometry. Mining Engineering, 11, 1145-1151.

Ray, J. R., 1930. Sulfide replacement o fore minerals. Econ. Geol., 25, 433-451.

Schouten, C., 1934. Structures and textures of synthetic replacement in "Open Space". Econ. Geol., 29, 611-658.

Schwartz, G. M., 1931. Textures due to un-mixing of solid solutions. Econ. Geol., 26, 739-763.

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Published

1994-11-30

How to Cite

Shah, M. T. (1994). A note on the bornite-chalcopyrite intergrowth texture in the volcanic-hosted copper mineralization in the Dir area, northern Pakistan. Journal of Himalayan Earth Sciences, 27(1), 125-126. Retrieved from http://ojs.uop.edu.pk/jhes/article/view/1466

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