Abstract
Since the tin deposits show accumulations of those minerals usually called pneumatolitic, it is beyond all doubt that their genesis is closely related to the intrusion of the granitic magma 1).
The erratum of this chapter is available at http://dx.doi.org/10.1007/978-94-015-7553-9_40
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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_13
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DOI: https://doi.org/10.1007/978-94-015-7553-9_13
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