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Trace Element Geochemistry of Alluvial TiO2 Polymorphs as a Proxy for Sn and W Deposits

dc.contributor.authorGaspar, Miguel
dc.contributor.authorGrácio, Nuno
dc.contributor.authorSalgueiro, Rute
dc.contributor.authorCosta, Mafalda
dc.date.accessioned2022-11-30T12:42:13Z
dc.date.available2022-11-30T12:42:13Z
dc.date.issued2022-10
dc.description.abstractABSTRACT: The Segura mining field, the easternmost segment of the Gois-Panasqueira-Segura tin-tungsten metallogenic belt (north-central Portugal), includes Sn-W quartz veins and Li-Sn aplite-pegmatites, which are believed to be genetically related to Variscan Granites. Sediment geochemistry indicates granite-related Ti-enrichments, locally disturbed by mineralization, suggesting magmatic and metamorphic/metasomatic titaniferous phases. Therefore, Segura alluvial samples and the geochemistry of their TiO2 polymorphs (rutile, anatase, and brookite) were investigated, and their potential as exploration tools for Sn and W deposits was evaluated. The heavy-mineral assemblages proved to be good proxies for bedrock geology, and TiO2 polymorph abundances were found to be suitable indicators of magmatic and/or metasomatic hydrothermal processes. The trace element geochemistry of Segura's alluvial rutile, anatase, and brookite is highly variable, implying multiple sources and a diversity of mineral-forming processes. The main compositional differences between TiO2 polymorphs are related to intrinsic (structural) factors, and to the P-T-X extrinsic parameters of their forming environments. Anomalous enrichments, up to 9% Nb, 6% Sn and W, 3% Fe, 2% Ta, and 1% V in rutile, and up to 1.8% Fe, 1.7% Ta, 1.2% Nb, 1.1% W 0.5% Sn and V in anatase, were registered. Brookite usually has low trace element content (<0.5%), except for Fe (similar to 1%). HFSE-rich and granitophile-rich rutile is most likely magmatic, forming in extremely differentiated melts, with Sn and W contents enabling the discrimination between Sn-dominant and W-dominant systems. Trace element geochemical distribution maps show pronounced negative Sn (rutile+anatase) and W (rutile) anomalies linked to hydrothermal cassiterite precipitation, as opposed to their hydrothermal alteration halos and to W-dominant cassiterite-free mineralized areas, where primary hydrothermal rutile shows enrichments similar to magmatic rutile. This contribution recognizes that trace element geochemistry of alluvial TiO2 polymorphs can be a robust, cost- and time-effective, exploration tool for Sn(W) and W(Sn) ore deposit systems.pt_PT
dc.description.versioninfo:eu-repo/semantics/publishedVersionpt_PT
dc.identifier.citationGaspar, Miguel... [et.al.] - Trace Element Geochemistry of Alluvial TiO2 Polymorphs as a Proxy for Sn and W Deposits. In: Minerals, 2022, vol. 12(10), article nº 1248pt_PT
dc.identifier.doi10.3390/min12101248pt_PT
dc.identifier.eissn2075-163X
dc.identifier.urihttp://hdl.handle.net/10400.9/3965
dc.language.isoengpt_PT
dc.peerreviewedyespt_PT
dc.publisherMDPIpt_PT
dc.relationInstituto Dom Luiz
dc.relationHERCULES Laboratory - Cultural Heritage, Studies and Safeguard
dc.relationHERCULES Laboratory - Cultural Heritage, Studies and Safeguard
dc.relation.publisherversionhttps://doi.org/10.3390/min12101248pt_PT
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/pt_PT
dc.subjectHeavy mineralspt_PT
dc.subjectTitanium dioxidept_PT
dc.subjectPolymorphspt_PT
dc.subjectAlluvialpt_PT
dc.subjectGeochemistrypt_PT
dc.subjectGeochemical explorationpt_PT
dc.titleTrace Element Geochemistry of Alluvial TiO2 Polymorphs as a Proxy for Sn and W Depositspt_PT
dc.typejournal article
dspace.entity.typePublication
oaire.awardTitleInstituto Dom Luiz
oaire.awardTitleHERCULES Laboratory - Cultural Heritage, Studies and Safeguard
oaire.awardTitleHERCULES Laboratory - Cultural Heritage, Studies and Safeguard
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDB%2F50019%2F2020/PT
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDB%2F04449%2F2020/PT
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDP%2F04449%2F2020/PT
oaire.awardURIinfo:eu-repo/grantAgreement/FCT/3599-PPCDT/ERA-MIN%2F0002%2F2019/PT
oaire.citation.titleMineralspt_PT
oaire.citation.volume12pt_PT
oaire.fundingStream6817 - DCRRNI ID
oaire.fundingStream6817 - DCRRNI ID
oaire.fundingStream6817 - DCRRNI ID
oaire.fundingStream3599-PPCDT
person.familyNameGaspar
person.familyNameGrácio
person.familyNameSalgueiro
person.familyNameBarrocas Dias Teixeira da Costa
person.givenNameMiguel
person.givenNameNuno
person.givenNameRute
person.givenNameMafalda
person.identifier2406151
person.identifier.ciencia-idF31A-64CB-F34D
person.identifier.ciencia-id1813-25D8-EA31
person.identifier.ciencia-idB01D-A767-9FD0
person.identifier.orcid0000-0003-2363-2919
person.identifier.orcid0000-0001-5825-2508
person.identifier.orcid0000-0002-3740-2965
person.identifier.orcid0000-0001-8764-2310
person.identifier.ridA-2403-2013
person.identifier.scopus-author-id7102412203
person.identifier.scopus-author-id57013986300
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.identifierhttp://doi.org/10.13039/501100001871
project.funder.nameFundação para a Ciência e a Tecnologia
project.funder.nameFundação para a Ciência e a Tecnologia
project.funder.nameFundação para a Ciência e a Tecnologia
project.funder.nameFundação para a Ciência e a Tecnologia
rcaap.rightsopenAccesspt_PT
rcaap.typearticlept_PT
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