As the hydrothermal alteration zones exist widely in the Oruro-Uyuni region and also mineral showings exist, it is expected to host epithermal ore deposits at depth. Considering the mineralization in the Altiplano and the Eastern Bolivian Andes, it was interpreted that the mineralization in the Western Bolivian Andes is similar to the Bolivian-type deposit and shows an epithermal type mineralization in the upper part, while it changes to a polymetallic mineralization in the lower part. It is reported that the mineralized ages of Chilean porphyry type deposits have a tendency to become younger from west to east and the porphyry type deposits were expected. Sixteen Districts were studied in three years. After the surveys lots of matters about the mineralizations in the Oruro-Uyui region still remained unknown, nevertheless the following things became clea
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