CONCHITA MINE (ESTEPONA)
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Small adit worked for tungsten-bismuth-tellurium ores embedded in dolomitic marble, leucogranites gneisses and pegmatitic sequences overlying alpine peridotites.
Origin: Magnesium Skarn in Triassic marbles with chondrodite-serpentine association, and late mineralizing fluids infillings Cretaceous karst (Atanores-Pipes)