Genetic relationships between Fe-Mn ores in the Cuera Range (Cantabrian Mountains, NW Spain)

Authors

  • Brais Gonzalo Guerra Departamento de Geología, Universidad de Oviedo. - Instituto Geológico y Minero de España (IGME-CSIC), Oviedo.
  • Nemesio Heredia Carballo Geological Survey of Spain
  • Pedro Farias Arquer University of Oviedo, Department of Geology

DOI:

https://doi.org/10.55407/geogaceta98165

Keywords:

Fe-Mn, ore-generation, fluid-flow, normal-fault, ore-type

Abstract

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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Published

2023-12-18

How to Cite

Gonzalo Guerra, B., Heredia Carballo, N., & Farias Arquer, P. (2023). Genetic relationships between Fe-Mn ores in the Cuera Range (Cantabrian Mountains, NW Spain). GEOGACETA, 74, 119–122. https://doi.org/10.55407/geogaceta98165

Issue

Section

Artículos