Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/59956
DC FieldValueLanguage
dc.contributor.authorMenéndez González, Inmaculadaen_US
dc.contributor.authorCampeny, Marcen_US
dc.contributor.authorQuevedo-Gonzalez, Luisen_US
dc.contributor.authorMangas Viñuela, Joséen_US
dc.contributor.authorLlovet, Xavieren_US
dc.contributor.authorTauler, Esperancaen_US
dc.contributor.authorBarron, Vidalen_US
dc.contributor.authorTorrent, Joseen_US
dc.contributor.authorMéndez-Ramos, Jorgeen_US
dc.date.accessioned2019-12-20T12:37:38Z-
dc.date.available2019-12-20T12:37:38Z-
dc.date.issued2019en_US
dc.identifier.issn0375-6742en_US
dc.identifier.otherWoS-
dc.identifier.urihttp://hdl.handle.net/10553/59956-
dc.description.abstractGran Canaria is a hotspot-derived, intraplate, oceanic island, comprising a variety of alkaline felsic magmatic rocks (i.e. phonolites, trachytes, rhyolites and syenites). These rocks are enriched in rare-earth elements (REE) in relation to the mean concentration in the Earth's crust and they are subsequently mobilised and redistributed in the soil profile. From a set of 57 samples of felsic rocks and 12 samples from three paleosol profiles, we assess the concentration and mobility of REE. In the saprolite that developed over the rhyolites, we identified REE-bearing minerals such as primary monazite-(Ce), as well as secondary phases associated with the edaphic weathering, such as rhabdophane-(Ce) and LREE oxides. The averaged concentration of REE in the alkaline bedrock varies from trachytes (449 mg kg(-1)), to rhyolites (588 mg kg(-1)) and to phonolites (1036 mg kg(-1)). REE are slightly enriched in saprolites developed on trachyte (498 mg kg(-1)), rhyolite (601 mg kg(-1)) and phonolite (1171 mg kg(-1)) bedrocks. However, B-horizons of paleosols from trachytes and phonolites showed REE depletion (436 and 994 mg kg(-1), respectively), whereas a marked enrichment was found in soils developed on rhyolites (1584 mg kg(-1)). According to our results, REE resources on Gran Canaria are significant, especially in Miocene alkaline felsic magmatic rocks (declining stage) and their associated paleosols. We estimate a total material volume of approximately 1000 km(3) with REE concentrations of 672 +/- 296 mg kg(-1), yttrium contents of 57 +/- 30 mg kg(-1), and light and heavy REE ratios (LREE/HREE) of 17 +/- 6. This mineralisation can be considered as bulk tonnage and low-grade ore REE deposits but it remains necessary to develop detailed mineral exploration on selected insular zones in the future, without undermining environmental and socioeconomic interests.en_US
dc.languageengen_US
dc.relation.ispartofJournal of Geochemical Explorationen_US
dc.sourceJournal Of Geochemical Exploration [ISSN 0375-6742], v. 204, p. 270-288en_US
dc.subject250611 Mineralogíaen_US
dc.subject.otherTrace-Elementsen_US
dc.subject.otherChemical Classificationen_US
dc.subject.otherWeathering Profileen_US
dc.subject.otherFractionationen_US
dc.subject.otherGeochemistryen_US
dc.subject.otherREE-bearing mineralsen_US
dc.subject.otherMineralizationen_US
dc.subject.otherDissolutionen_US
dc.subject.otherPhosphateen_US
dc.subject.otherComplexen_US
dc.subject.otherREE explorationen_US
dc.subject.otherWeathering processesen_US
dc.subject.otherOcean intraplate volcanic islandsen_US
dc.subject.otherGran Canaria (Canary Islands)en_US
dc.titleDistribution of REE-bearing minerals in felsic magmatic rocks and paleosols from Gran Canaria, Spain: Intraplate oceanic islands as a new example of potential, non-conventional sources of rare-earth elementsen_US
dc.typeinfo:eu-repo/semantics/Articleen_US
dc.typeArticleen_US
dc.identifier.doi10.1016/j.gexplo.2019.06.007
dc.identifier.scopus85068035882
dc.identifier.isi000477711700019-
dc.contributor.authorscopusid6701688947
dc.contributor.authorscopusid15071510500
dc.contributor.authorscopusid57208513173
dc.contributor.authorscopusid56114334400
dc.contributor.authorscopusid6603693732
dc.contributor.authorscopusid24287022600
dc.contributor.authorscopusid7003440812
dc.contributor.authorscopusid7006586226
dc.contributor.authorscopusid6602563211
dc.identifier.eissn1879-1689-
dc.description.lastpage288-
dc.description.firstpage270-
dc.relation.volume204-
dc.investigacionCienciasen_US
dc.type2Artículoen_US
dc.contributor.daisngid30771427
dc.contributor.daisngid30720177
dc.contributor.daisngid31054978
dc.contributor.daisngid1765426
dc.contributor.daisngid554845
dc.contributor.daisngid24688117
dc.contributor.daisngid275838
dc.contributor.daisngid67705
dc.contributor.daisngid463558
dc.utils.revisionen_US
dc.contributor.wosstandardWOS:Menendez, I
dc.contributor.wosstandardWOS:Campeny, M
dc.contributor.wosstandardWOS:Quevedo-Gonzalez, L
dc.contributor.wosstandardWOS:Mangas, J
dc.contributor.wosstandardWOS:Llovet, X
dc.contributor.wosstandardWOS:Tauler, E
dc.contributor.wosstandardWOS:Barron, V
dc.contributor.wosstandardWOS:Torrent, J
dc.contributor.wosstandardWOS:Mendez-Ramos, J
dc.date.coverdateSeptiembre 2019
dc.identifier.ulpgces
dc.description.sjr0,839
dc.description.jcr3,352
dc.description.sjrqQ1
dc.description.jcrqQ2
dc.description.scieSCIE
item.grantfulltextnone-
item.fulltextSin texto completo-
crisitem.author.deptGIR IOCAG: Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.deptGIR IOCAG: Geología Aplicada y Regional-
crisitem.author.deptIU de Oceanografía y Cambio Global-
crisitem.author.deptDepartamento de Física-
crisitem.author.orcid0000-0002-1801-5177-
crisitem.author.orcid0000-0002-3286-743X-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.parentorgIU de Oceanografía y Cambio Global-
crisitem.author.fullNameMenéndez González, Inmaculada-
crisitem.author.fullNameMangas Viñuela, José-
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