In this communication, we will do a brief description of the cupriferous mineralizations associated to the red-beds, and placed between the sandy stretch of Inferior Triassic, in the municipal terms of Olesa de Montserrat and Esparraguera, in the district of the Baix LLobregat, in the region of Barcelona, in Catalunya. These mineralizations are placed between the materials that take part of the Serralada Prelitoral Catalana, in the Cadena Costanera Catalana, in the contiguities of the Llobregat River
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