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Location: 110 km E from Copiapo, Chile
Lo Fontecilla 101 Office 716 Las CondesSantiago de ChileChile
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Francisco Basin is classified as an immature clastic salar characterised by greater moisture regimes and a sediment profile with higher porosities than mature halite salars. The Francisco Basin is an elongated basin aligned on a NW-SE axis bounded on all sides by volcanic mountain ranges. The surface of the salar is at an elevation of approximately 4,136m. To the south-east the basin forms a gently rising plain which forms the focus area of the project. The basin fill is characterised by sedimentary deposits that can be separated into three general units:1. An upper unit of fine to coarse sands intercalated with fine gravels, minor clay and tuff levels 2. A middle unit of clay beds intercalated with minor levels of fine sands and gypsum 3. A basal unit of moderately consolidated gravels and sands, transitioning to silt bedsThe brine aquifer is contained mainly from the middle unit down to the basement.DimensionsThe Brine Resource is a sub horizontal lens with an approximately area of 9 km x 5 km and 320 m wide