@article{jgg2015342,
author={{A., Ako T. and Vishiti, A. and Ateh, K. I. and Kedia, A. C. and Suh, C. E.},
title={Mineral Alteration and Chlorite Geothermometry in Platinum Group Element (PGE)- Bearing Meta-ultramafic Rocks from South East Cameroon},
journal={Journal of Geosciences and Geomatics},
volume={3},
number={4},
pages={96--108},
year={2015},
url={http://pubs.sciepub.com/jgg/3/4/2},
issn={2373-6704},
abstract={The meta-ultramafic rocks that are part of the Paleoproterozoic unit termed the Nyong Series in SE Cameroon were investigated in this study. The lithologic assemblage mapped is exposed on a cliff face and consists of distinguishable horizons that include least, moderately to intensely altered pyroxenite to amphibolite units. The rocks are partially to completely serpenitinized and foliated. The main mineral phases identified under the microscope include pyroxenes (clinopyroxene and orthopyroxene), olivine, hornblende, plagioclase, garnet and sulphides. The rocks depict variable alteration of the pyroxenes and other primary minerals such as olivine to actinolite, chlorite, serpentine, talc, epidote and tremolite. Electron microprobe analysis on chlorite show that the principal chlorite type ranges from talc-chlorite to penninite. Using the chlorite geothermometer it is observed that the hydrothermal alteration temperatures vary between 160-180ˇăC. This has been overprinted by surface temperatures (20 - 40ˇăC) during the process of weathering.},
doi={10.12691/jgg-3-4-2}
publisher={Science and Education Publishing}
}