Relaciones genéticas entre yacimientos de Fe-Mn en la Sierra del Cuera (Cordillera Cantábrica, NO de España)
- Brais Gonzalo-Guerra 1
- Nemesio Heredia 2
- Pedro Farias 1
- 1 Universidad de Oviedo, Departamento de Geología, Oviedo
- 2 Instituto Geológico y Minero de España (IGME-CSIC), Oviedo
ISSN: 0213-683X
Year of publication: 2023
Issue: 74
Pages: 119-122
Type: Article
More publications in: Geogaceta
Abstract
This paper describes three different Fe-Mn ore-types found in Cuera Range (Cantabrian Mountains, NW Spain): Sedimentary (Carboniferous), low-temperature hydrothermal (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, FeMn was remobilized by a hydrothermal event and, eventually, FeMn was reconcentrated by recent karstic processes.