Las mineralizaciones litiniferas del oeste de Salamanca y Zamora
DOI:
https://doi.org/10.3989/egeol.92481-2367Keywords:
Lithium, pegmatites, veins, ore deposits, HercynianAbstract
The aim of this paper is to describe the most important geological, mineralogical and geochemical features of the Li ores (bouth pegmatites and quartz veins) located in the west part of the Salamanca and Zamora provinces. The pegmatites mostly belong to the lepidolite type and they are complex and zoned. In one case, the ore in the pegmatite is litiophilite, and the pegmatite is simple. The veins are quartz rich with ambligonite and sorne feldspar and sulphides. They appear always related to granitic rocks. All these bodies are also mineralized with cassiterite, and sorne of them contain columbite tantalite too.
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Published
1992-04-30
How to Cite
Martín-Izard, A., Reguilón, R., & Palero, F. (1992). Las mineralizaciones litiniferas del oeste de Salamanca y Zamora. Estudios Geológicos, 48(1-2), 19–30. https://doi.org/10.3989/egeol.92481-2367
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