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Iron and lead-antimony masses are inside dolomites and brecciated dolomites belonging to Sierra de las Nieves Unit, Triassic age. The deposit has a interesting formation regarding geological conditions as karst and sediments in conjunction with primary ores were reworked by tectonic settings (low angle faults)during alpine orogeny.
10 entries listed. 8 valid minerals.
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- Romero Silva, J.C. (2003): Minerales y Rocas de la provincia de Málaga. Diputación de Málaga, 318 pp.