This document summarizes uranium exploration results in the Paraná Basin of Paraguay. It provides geological context, including the stratigraphy and tectonic setting. It then describes both historic and current exploration efforts that have identified uranium mineralization, particularly along fault zones, within the San Miguel Formation. Preliminary pumping tests suggest the mineralization could be amenable to in-situ recovery. The results indicate the potential for uranium deposits in the basin.
8. Geologic Setting: Stratigraphic Section
• Alto Paraná Fm
– Alkaline intrusives
• San Miguel Fm
– Deltaic, fluvial, etc.
sandstones (U host)
• Coronel Oviedo Fm
– Glacial, fluvial, and marine
sediments
After Baretto, 1985, and Fulfaro, 1996
11. Historic Exploration: Anschutz
Corporation
• 1976 – 1983 joint venture with:
Korea Electro Power Company (KEPCO)
Taiwan Power Company (TPC)
• 162,000 km2 – all eastern Paraguay
• Airborne radiometric and magnetic surveys
• San Miguel Formation
Massive Sand Unit
Fine-grained Sand Unit
Wavy Unit
23. Current Exploration:
Coronel Oviedo
Tres Corrales pumping test
Mineralized zone confined and
saturated
+ 48 gallons/minute yield
= ISR amenability
Similar to S. Texas and Wyoming
25. Paragenesis
• Roll front
• South Texas Coastal Plain style of uranium mineralization
• Environment: coastal plain coalescing paleochannels
• Uranium sources:
Continued leaching of underlying sediments
Overlying K alkaline intrusives
• Reductants: organic material in sands,
hydrocarbon-related gases
South Texas coastal plain NAIP imagery 2010
26. Summary and Conclusions
• Paraná Basin hosts mineralized strata
– Brazil: Rio Bonito
– Paraguay: San Miguel
• Extensive historic database
• Current exploration results
– Mineralization concentrated along faults
~60mm
– ISR amenable deposits
• Possible re-reduction masking