Abstract
As stanniferous veins are invariably associated with the formation of tourmaliniferous phyllites or schists, only these rocks will be discussed here. Moreover the omission of other types of contact metamorphic rocks is fully justified, as they do not show any remarkable features.
The erratum of this chapter is available at http://dx.doi.org/10.1007/978-94-015-7553-9_44
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© 1932 Springer Science+Business Media Dordrecht
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Stheeman, H.A. (1932). Sericite Phyllites in the Vicinity of Granite. In: The Geology of Southwestern Uganda. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-7553-9_17
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DOI: https://doi.org/10.1007/978-94-015-7553-9_17
Publisher Name: Springer, Dordrecht
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