Major-element analysis of the La Alquimia Compañía Anónima rock collection: Establishing a geochemical repository for the systematic classification of Iberian karstic bauxite and kaolin deposits

dc.contributor.authorRoqué, Josep
dc.contributor.authorIbáñez-Insa, Jordi
dc.contributor.authorGranado, Pablo
dc.contributor.authorMartín, Juan Diego (Martín Martín)
dc.contributor.authorÁlvarez-Pousa, Soledad
dc.contributor.authorCerdà i Domènech, Marc
dc.contributor.authorJiménez-Franco, Abigail
dc.date.accessioned2025-04-24T12:05:04Z
dc.date.available2025-04-24T12:05:04Z
dc.date.issued2025-04-02
dc.date.updated2025-04-24T12:05:04Z
dc.description.abstractThe company La Alquimia Compañía Anónima rock collection comprises a wide range of samples from karstic bauxites to kaolin deposits across the Iberian Peninsula. Collected during mid-20th-century prospecting efforts, aimed to identify bauxites for exploitation and aluminum oxide production, this rock collection offers an unprecedented opportunity to perform a systematic study of some of the most important Iberian karstic bauxite and kaolin deposits. The major-element data from the samples were obtained through handheld X-ray fluorescence (XRF) and analyzed using Principal Components Analysis (PCA), revealing SiO2 and Al2O3 as the key components that explain the most variance. The XRF data confirmed that the samples mostly consist of karstic bauxites and kaolin, with minor amounts of gibbsite and alunite deposits. The calculated Index Of Laterization/Index Of Bauxitization (IOL/IOB) and Chemical Index of Alteration (CIA), and the SiO2 – Al2O3 – Fe2O3 and Al2O3 – CaO*+Na2O – K2O ternary diagrams have facilitated the categorization of karstic bauxites into 'bauxitic' and 'lateritic' types, and the kaolin deposits into 'gabbro' and 'granite' derived types with an intermediate to extreme degrees of weathering. The data highlights potential differences in formation settings possibly influenced by regional factors such as volcanism and tectonics, as well as global factors like eustasy and climate, which could explain the compositional disparities observed in the Iberian karstic bauxites and kaolin deposits.
dc.format.extent13 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec758186
dc.identifier.issn1695-6133
dc.identifier.urihttps://hdl.handle.net/2445/220576
dc.language.isoeng
dc.publisher(UB). (ICTJA). (IDEA). (UAB). (CSIC)
dc.relation.isformatofReproducció del document publicat a: https://doi.org/DOI: 10.1344/GeologicaActa2025.23.8
dc.relation.ispartofGeologica Acta, 2025, vol. 23, p. 1-13
dc.relation.urihttps://doi.org/DOI: 10.1344/GeologicaActa2025.23.8
dc.rightscc-by-sa (c) Roqué-Rosell, J. et al., 2025
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-sa/4.0/
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject.classificationClassificació de les roques
dc.subject.classificationBauxita
dc.subject.classificationMinerals d'argila
dc.subject.classificationPenínsula Ibèrica
dc.subject.classificationGeoquímica
dc.subject.classificationCaolí
dc.subject.classificationEspectroscòpia de raigs X
dc.subject.otherClassification of rocks
dc.subject.otherBauxite
dc.subject.otherClay minerals
dc.subject.otherIberian Peninsula
dc.subject.otherGeochemistry
dc.subject.otherKaolin
dc.subject.otherX-ray spectroscopy
dc.titleMajor-element analysis of the La Alquimia Compañía Anónima rock collection: Establishing a geochemical repository for the systematic classification of Iberian karstic bauxite and kaolin deposits
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion

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