Mineralogical evolution of the Las Cruces gossan cap (Iberian Pyrite Belt): From subaerial to underground conditions
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First detailed mineralogical study of the uncommon Las Cruces weathered cap (Iberian Pyrite Belt)

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Description of mineral associations and its evolution from subaerial to underground conditions

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Role of carbonated sedimentary cover and the water-rock interaction processes

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Role of Alpine rejuvenated Variscan-fault for basinal fluids circulation and mineralogenesis

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