With the WATEX™ Mineral Mapping solution, it is possible to gain a thorough understanding of subsurface geology, particularly in relation to geothermal sites, which is crucial for the exploration of Rare Earths and Lithium.
CONTEXT
The considerable geological and geochemical work achieved by specialists involved in exploration since 1912 lead to the understanding that orebodies from this area of Madagascar are more related to carbonatites intrusions rather than pegmatites.
Their Rare Earths Elements (REE) components share similar characteristics with the Mountain Pass Carbonatites of Nevada, USA.
The sum of REE of these sites ranges from 4 to 12 % and are composed of oxides of Cerium (40–45 %), Lanthanum (33–41 %), Neodymium (11–14 %) with a considerable content of Scandium (0.63–5.10 %). Oxides of Praseodymium, Samarium, Europium, Cadmium, Dysprosium and Erbium are present, as well as negligible quantities of Holmium, Thulium, Ytterbium and Lutetium.
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