Caracterización geoquímica preliminar de los metatasedimentos ordovicicos del sinforme de Alcanices (Zamora)
DOI:
https://doi.org/10.3989/egeol.93495-6358Keywords:
Ordovician metasediments, Fe mineralizations, geochemistry, Alcañices SynformAbstract
The geochemistry of the Ordovician metasediments and associated Fe sedimentary mineralizations of the South limb of the Alcañices Synform suggest a siliceous nature for the Cabeza de las Viñas (pre-Arenigian) and Pielgo Quartzite (Arenigian) Formations as compared with the essentially aluminic character of the Latedo (Llanvirnian-Llandeilian) Formation and a sediment essentially formed of Fe oxyhydroxides, quartz and clay minerals as precursors of the Fe mineralizations.
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