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Contrasting high‑Mg, high‑K rocks in Central Iberia: the appinite—vaugnerite conundrum and their (non‑existent) relation with arc magmatism

dc.contributor.authorBea, F.
dc.contributor.authorGallastegui, G
dc.contributor.authorMontero, P.
dc.contributor.authorMolina, J. F.
dc.contributor.authorScarrow, J.
dc.contributor.authorCuesta Fernández, Andrés 
dc.contributor.authorGonzález Menéndez, Luis
dc.date.accessioned2021-02-25T13:12:35Z
dc.date.available2021-02-25T13:12:35Z
dc.date.issued2020
dc.identifier.citationJournal of Iberian Geology, 47, p. 235-261 (2020); doi:10.1007/s41513-020-00152-x
dc.identifier.issn1698-6180
dc.identifier.issn1886-7995
dc.identifier.urihttp://hdl.handle.net/10651/58060
dc.description.sponsorshipThis is the IBERSIMS manuscript nº 76 financially supported by the Spanish Grant CGL2017-84469-P.spa
dc.format.extentp. 235-261
dc.language.isoengspa
dc.relation.ispartofJournal of Iberian Geologyspa
dc.rights© 2021, Universidad Complutense de Madrid
dc.rightsCC Reconocimiento - No Comercial - Sin Obra Derivada 4.0 Internacional
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.titleContrasting high‑Mg, high‑K rocks in Central Iberia: the appinite—vaugnerite conundrum and their (non‑existent) relation with arc magmatismspa
dc.typejournal articlespa
dc.identifier.doi10.1007/s41513-020-00152-x
dc.relation.projectIDCGL2017-84469-Pspa
dc.relation.publisherversionhttp://dx.doi.org/10.1007/s41513-020-00152-xspa
dc.rights.accessRightsopen access
dc.type.hasVersionAM


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