Relaciones genéticas entre yacimientos de Fe-Mn en la Sierra del Cuera (Cordillera Cantábrica, NO de España)

  1. Brais Gonzalo-Guerra 1
  2. Nemesio Heredia 2
  3. Pedro Farias 1
  1. 1 Universidad de Oviedo
    info
    Universidad de Oviedo

    Oviedo, España

    ROR https://ror.org/006gksa02

    Situation géographique de l'organisation Universidad de Oviedo
  2. 2 Instituto Geológico y Minero de España
    info
    Instituto Geológico y Minero de España

    Madrid, España

    ROR https://ror.org/04cadha73

    Situation géographique de l'organisation Instituto Geológico y Minero de España
Revue:
Geogaceta

ISSN: 0213-683X

Année de publication: 2023

Número: 74

Pages: 119-122

Type: Article

DOI: 10.55407/GEOGACETA98165 DIALNET GOOGLE SCHOLAR lock_openAccès ouvert editor

D'autres publications dans: Geogaceta

Objectifs de Développement Durable

Résumé

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.

La source de données: Dialnet