![Sample our Earth Sciences journals, sign in here to start your access, latest two full volumes FREE to you for 14 days]({"type":"image" , "src" : "/sda/5930/TOC-Subject-Sample-2021-Earth-Sciences.jpg"})
The tin mineralization at Rondonia, W. Brazil, is characterized by the association cassiterite and topaz. Both minerals occur as replacements in Precambrian to Early Paleozoic granites. The tin mineralization of the Eastern Cordilleras of Bolivia, on the other hand, has cassiterite and tourmaline as characteristic mineral association, and is related to the occurence of large granitic batholiths. The origin of the two tin mineralizations is discussed.
Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?
To request a reprint or corporate permissions for this article, please click on the relevant link below:
Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?
Obtain permissions instantly via Rightslink by clicking on the button below:
If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.
