dc.contributor.author
Domínguez-Carretero, Diego
dc.contributor.author
Villanova de Benavent, Cristina
dc.contributor.author
Torró i Abat, Lisard
dc.contributor.author
Pujol Solà, Núria
dc.contributor.author
Bover-Arnal, Telm
dc.contributor.author
Mestre, Àngel
dc.contributor.author
Aiglsperger, Thomas Hans
dc.contributor.author
Ramírez, Australia
dc.contributor.author
Rodríguez, Jesús
dc.contributor.author
Espaillat, Julio
dc.contributor.author
Proenza Fernández, Joaquín Antonio
dc.date.accessioned
2025-11-19T10:53:04Z
dc.date.available
2025-11-19T10:53:04Z
dc.date.issued
2025-09-10T07:14:39Z
dc.date.issued
2025-09-10T07:14:39Z
dc.date.issued
2025-05-01
dc.date.issued
2025-09-10T07:14:39Z
dc.identifier
https://hdl.handle.net/2445/223084
dc.identifier.uri
https://hdl.handle.net/2445/223084
dc.description.abstract
The energy transition, which aims to reduce carbon emissions and to slow down climate change, demands an ever-increasing supply of the so-called “critical metals”. Rare-earth elements and yttrium (REY) are among the most critical metals, as they are indispensable in most technologies associated with the generation and storage of renewable energy. In recent years there has been a growing interest in the potential of karst bauxites as non-conventional sources of REY and other critical metals such as Sc and Ga. The Sierra de Bahoruco (SW Dominican Republic) contains the most REY-enriched karst bauxites globally. In view of the high potential for hosting important REY contents, the Dominican Republic government has declared the Reserva Fiscal Ávila (RFA), a state-owned area within the Sierra de Bahoruco for assessment and exploration of its REY resources. In this study, we present the first data on the mineralogy and composition of bauxitic rocks from the RFA. The bauxitic deposits comprise clayey bauxites and Fe-rich bauxites that are composed predominantly of Al-oxyhydroxides (gibbsite, boehmite and nordstrandite), kaolinite and Fe-oxyhydroxides. The bauxites are enriched in REY, with a median value of 1,310ppm and up to 2,542ppm, with a consistent enrichment in light REE (LREE) and Y compared to middle (MREE) and heavy REE (HREE). The positive correlation between the contents of REY and Th, and negative correlation with K, makes gamma-ray spectrometry an appropriate tool for the exploration. In addition, bauxitic rocks from the RFA contain significant Sc (up to 105ppm) and Ga (up to 54ppm) contents, and their extraction could potentially represent a substantial economic surplus to the revenue generated solely from the aluminum production. Based on the trace element geochemistry, we suggest that Karst bauxite deposits from the Reserva Fiscal Ávila bauxites from the RFA had a similar parental source to the soils and bauxites from Jamaica.
dc.format
application/pdf
dc.format
application/pdf
dc.publisher
(UB). (ICTJA). (IDEA). (UAB). (CSIC)
dc.relation
Reproducció del document publicat a: https://doi.org/10.1344/GeologicaActa2025.23.9
dc.relation
Geologica Acta, 2025, vol. 23, p. 1-18
dc.relation
https://doi.org/10.1344/GeologicaActa2025.23.9
dc.rights
cc-by-sa (c) Domínguez-Carretero, Diego et al., 2025
dc.rights
http://creativecommons.org/licenses/by-sa/4.0/
dc.rights
info:eu-repo/semantics/openAccess
dc.source
Articles publicats en revistes (Mineralogia, Petrologia i Geologia Aplicada)
dc.subject
República Dominicana
dc.subject
Dominican Republic
dc.title
Mineralogy, geochemistry and origin of karst bauxite deposits from the Reserva Fiscal Ávila, SW Dominican Republic
dc.type
info:eu-repo/semantics/article
dc.type
info:eu-repo/semantics/publishedVersion