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.
Keywords
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
The erratum of this chapter is available at http://dx.doi.org/10.1007/978-94-015-7553-9_46
This is a preview of subscription content, log in via an institution.
Buying options
Tax calculation will be finalised at checkout
Purchases are for personal use only
Learn about institutional subscriptionsPreview
Unable to display preview. Download preview PDF.
Author information
Authors and Affiliations
Rights and permissions
Copyright information
© 1932 Springer Science+Business Media Dordrecht
About this chapter
Cite this chapter
Stheeman, H.A. (1932). Introduction. In: The Geology of Southwestern Uganda. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-7553-9_19
Download citation
DOI: https://doi.org/10.1007/978-94-015-7553-9_19
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-017-0021-4
Online ISBN: 978-94-015-7553-9
eBook Packages: Springer Book Archive