Genetic relationships between Fe-Mn ores in the Cuera Range (Cantabrian Mountains, NW Spain)
DOI:
https://doi.org/10.55407/geogaceta98165Keywords:
Fe-Mn, ore-generation, fluid-flow, normal-fault, ore-typeAbstract
This paper describes three different Fe-Mn ore-types found in Cuera Range (Cantabrian Mountains, NW Spain): Sedimentary (Carboniferous), Epithermal (early Permian) and Karstic supergene (Quaternary). Relationships between these ore-types have been analyzed, finding that they follow a temporary evolutive path: firstly, sedimentary ores were formed. Secondly, Fe-Mn was remobilized by a hydrothermal event and, eventually, Fe-Mn was reconcentrated by recent karstic processes.References
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Copyright (c) 2023 Brais Gonzalo Guerra, Nemesio Heredia Carballo, Pedro Farias Arquer
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