Critical elements in supergene phosphates: the example of the weathering profile at the Gavà Neolithic Mines, Catalonia, Spain

The essential role of Critical Elements (CE) in 21st century economy has led to an increasing demand of these metals and promotes the exploration of non-conventional deposits such as weathering profiles. The present work is focused on the study of a weathering profile located at the Archaeological P...

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Detalles Bibliográficos
Autores: Díaz-Acha, Yael, Campeny, Marc, Tauler, Esperança, Bosch, Josep, Melgarejo, Joan Carles, Camprubí, Antoni, Vilanova-de-Benavent, Cristina, Jorge-Villar, Susana E., Díaz-Ontiveros, Iria, Fernández-Lluch, David, Proenza, Joaquín A., Andreazini, Aleu, Pastor, Míriam
Tipo de recurso: artículo
Fecha de publicación:2019
País:España
Institución:Ajuntament de Barcelona
Repositorio:BCNROC. Repositori Obert de Coneixement de l'Ajuntament de Barcelona
OAI Identifier:oai:bcnroc.ajuntament.barcelona.cat:11703/120712
Acceso en línea:http://hdl.handle.net/2072/366988
https://doi.org/10.3390/min10010003
http://hdl.handle.net/11703/120712
Access Level:acceso abierto
Palabra clave:Gavà (Catalunya)
Fosfats
Can Tintorer (Gavà, Catalunya : Jaciment arqueològic)
Erosió
Ciència i tecnologia
articles
Descripción
Sumario:The essential role of Critical Elements (CE) in 21st century economy has led to an increasing demand of these metals and promotes the exploration of non-conventional deposits such as weathering profiles. The present work is focused on the study of a weathering profile located at the Archaeological Park of the Gavà Neolithic Mines, Barcelona, Catalonia, Spain. In the Gavà deposit, acid and oxidising meteoric fluids generated intense weathering during the early Pleistocene, affecting series of Llandoverian black shales and associated syn-sedimentary phosphates. The circulation of these acid fluids at deeper levels of the profile generated supergene vein-like mineralisations comprised of secondary phosphates (e.g., variscite, perhamite, crandallite, phosphosiderite) and sulphates (e.g., jarosite, alunite). This supergene mineralisation is significantly enriched in certain CE (e.g., Ga, Sc, REE, In, Co and Sb) that were mobilised from host rock components and later hosted in the crystal lattice of supergene minerals. Weathering processes and corresponding supergene enrichment of CE at the Gavà deposit could be used as an example to determine exploration guidelines of CE in weathering profiles and associated supergene phosphates worldwide. Keywords: critical elements; weathering; supergene mineralisation; phosphates; Gavà