Abstract
Oxygen Fugacity measurements were carried out on chromites from the Eastern Bushveld Complex (Maandagshoek) and are compared with former measurements on chromites from the western Bushveld Complex (Zwartkop Chrome Mine). These results together with those of Hill and Roeder (1974) yield the following conditions of formation for the massive chromitite layers:
Western Bushveld Complex (Zwartkop Chrome Mine)
Eastern Bushveld Complex (Farm Maandagshoek)
The comparison of the data shows, that the chronitite layers within each particular sequence were formed under approximately identicalp o 2- andT-conditions. The chromites from the western Bushveld Complex, however, were formed at higher temperatures and higher oxygen fugacities than the chromites from the eastern Bushveld Complex.
Fromp o 2-T-curves of disseminated chromites and the temperatures derived above, the following conditions of formation for the host rocks were obtained:
Western Bushveld Complex
Eastern Bushveld Complex
Consequently, the host rocks in the Zwartkop-Chrome-Mine, were formed under higher temperatures and higher oxygen fugacities than the host rocks at Maandagshoek. The rock sequence in the Zwartkop-Chrome-Mine therefore originated in an earlier stage of the differentiation of the Bushveld magma.
Comparison of the chromites from the host rocks with the chromites from massive layers supports Ulmer's (1969) thesis that an increase of the oxygen fugacity is responsible for the formation of massive chromitite layers. The values in this investigation show that increases of only about 0.5–1.0 log units are necessary to enhance chromitite layer formation.
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Snethlage, R., Klemm, D.D. Intrinsic oxygen Fugacity measurements on chromites from the Bushveld Complex and their petrogenetic significance. Contr. Mineral. and Petrol. 67, 127–138 (1978). https://doi.org/10.1007/BF01046571
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DOI: https://doi.org/10.1007/BF01046571