Abstract
In this part the additive processes will be described which are confined to the immediate vicinity of the main channels of the magmatic solutions. Particularly those processes will be discussed by which stanniferous veins have been formed.
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© 1932 Springer Science+Business Media Dordrecht
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Stheeman, H.A. (1932). Introduction. In: The Geology of Southwestern Uganda. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-7553-9_19
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DOI: https://doi.org/10.1007/978-94-015-7553-9_19
Publisher Name: Springer, Dordrecht
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