Publication
Ranked Mappable Criteria for Magmatic Units: Systematization of the Ossa-Morena Zone Rift-Related Alkaline Bodies
datacite.subject.fos | Ciências Naturais::Ciências da Terra e do Ambiente | |
datacite.subject.sdg | 13:Ação Climática | |
datacite.subject.sdg | 15:Proteger a Vida Terrestre | |
dc.contributor.author | Roseiro, José | |
dc.contributor.author | Moreira, Noel | |
dc.contributor.author | de Oliveira, Daniel Pipa Soares | |
dc.contributor.author | Silva, Marcelo | |
dc.contributor.author | Eguiluz, Luis | |
dc.contributor.author | Nogueira, Pedro | |
dc.date.accessioned | 2025-07-25T14:20:24Z | |
dc.date.available | 2025-07-25T14:20:24Z | |
dc.date.issued | 2025-02 | |
dc.description.abstract | ABSTRACT: The Ossa-Morena Zone (SW Iberian Massif) hosts the largest set of Cambro-Ordovician alkaline magmatic plutons related to the Palaeozoic rifting of the northern Gondwana margin so far described. An organized framework for their classification at different scales is proposed through data-driven ranks based on their distinctive petrological features relative to other rift-related magmatic rocks found throughout western Europe. The classification method aims to enhance geological mapping at different scales, regional- and continental-scale correlations, and, as such, facilitate the petrogenetic interpretation of this magmatism. The hierarchical scheme, from highest to lowest rank, is as follows: rank-1 (supersuite) assembles rocks that have distinctive characteristics from other magmatic units emplaced in the same magmatic event; rank-2 (suite) categorizes the units based on their major textural features, indicating if the body is plutonic, sub-volcanic, or a strongly deformed magmatic-derived unit; rank-3 (subsuite) clusters according to their spatial arrangement (magmatic centres) or association to larger structures (e.g., shear zones or alignments); rank-4, the fundamental mapping unit, characterizes the lithotype (alkaline granite, alkaline gabbro, syenite, albitite, etc.) by considering higher ranks (alkalinity and textural aspects); rank-5 characterizes the geometry of individual plutons (with several intrusions) or swarms; rank-6 (smallest mappable unit) corresponds to each intrusion or individual body from a swarm. Although this classification scheme is currently presented solely for the Ossa-Morena Zone, the scheme can be easily extended to incorporate other co-magmatic alkaline bodies, such as those in the NW Iberian allochthonous units or other peri-Gondwanan zones or massifs, in order to facilitate regional correlations of the rift-related magmatism. | eng |
dc.identifier.citation | Roseiro, J., Moreira, N., de Oliveira, D., Silva, M., Eguiluz, L. & Nogueira, P. (2025). Ranked Mappable Criteria for Magmatic Units: Systematization of the Ossa-Morena Zone Rift-Related Alkaline Bodies. In: Minerals, 2025, vol. 15 (2), article 174. https://doi.org/10.3390/min15020174 | |
dc.identifier.doi | 10.3390/min15020174 | |
dc.identifier.eissn | 2075-163X | |
dc.identifier.uri | http://hdl.handle.net/10400.9/6006 | |
dc.language.iso | eng | |
dc.peerreviewed | yes | |
dc.publisher | MDPI | |
dc.relation | From mantle to Iberia: crust-mantle interaction, geodynamic evolution and ore forming systems of alkaline melts in the northernmost Ossa-Morena Zone domains | |
dc.relation | Satélites e Veículos Aéreos Não-Tripulados trabalhando juntos no estudo de áreas degradadas | |
dc.relation | INSTITUTE OF EARTH SCIENCES | |
dc.relation.hasversion | https://www.mdpi.com/2075-163X/15/2/174 | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | |
dc.subject | Magmatic rocks | |
dc.subject | Lithologies | |
dc.subject | Ossa-Morena Zone | |
dc.subject | Iberian Massif | |
dc.subject | Mineralogy | |
dc.title | Ranked Mappable Criteria for Magmatic Units: Systematization of the Ossa-Morena Zone Rift-Related Alkaline Bodies | eng |
dc.type | journal article | |
dspace.entity.type | Publication | |
oaire.awardTitle | From mantle to Iberia: crust-mantle interaction, geodynamic evolution and ore forming systems of alkaline melts in the northernmost Ossa-Morena Zone domains | |
oaire.awardTitle | Satélites e Veículos Aéreos Não-Tripulados trabalhando juntos no estudo de áreas degradadas | |
oaire.awardTitle | INSTITUTE OF EARTH SCIENCES | |
oaire.awardURI | info:eu-repo/grantAgreement/FCT/POR_ALENT/UI%2FBD%2F150937%2F2021/PT | |
oaire.awardURI | http://hdl.handle.net/10400.9/6005 | |
oaire.awardURI | info:eu-repo/grantAgreement/FCT/6817 - DCRRNI ID/UIDB%2F04683%2F2020/PT | |
oaire.citation.issue | 2 | |
oaire.citation.title | Minerals | |
oaire.citation.volume | 15 | |
oaire.fundingStream | POR_ALENT | |
oaire.fundingStream | POR_ALENT | |
oaire.fundingStream | 6817 - DCRRNI ID | |
oaire.version | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |
person.familyName | Roseiro | |
person.familyName | Moreira | |
person.familyName | de Oliveira | |
person.familyName | Silva | |
person.familyName | Nogueira | |
person.givenName | José | |
person.givenName | Noel | |
person.givenName | Daniel Pipa Soares | |
person.givenName | Marcelo | |
person.givenName | Pedro | |
person.identifier | 2216267 | |
person.identifier.ciencia-id | CA15-6DEA-AECA | |
person.identifier.ciencia-id | 5310-3A9A-CA26 | |
person.identifier.ciencia-id | A11D-DDD7-29F2 | |
person.identifier.ciencia-id | 141D-B380-BCA7 | |
person.identifier.orcid | 0000-0003-3643-9122 | |
person.identifier.orcid | 0000-0003-0415-1474 | |
person.identifier.orcid | 0000-0002-6338-8845 | |
person.identifier.orcid | 0000-0001-6702-5753 | |
person.identifier.orcid | 0000-0002-6162-0030 | |
person.identifier.rid | J-1537-2016 | |
person.identifier.rid | I-9678-2017 | |
person.identifier.scopus-author-id | 57218627617 | |
person.identifier.scopus-author-id | 36170825600 | |
person.identifier.scopus-author-id | 12793083600 | |
project.funder.identifier | http://doi.org/10.13039/501100001871 | |
project.funder.identifier | http://doi.org/10.13039/501100001871 | |
project.funder.name | Fundação para a Ciência e a Tecnologia | |
project.funder.name | Fundação para a Ciência e a Tecnologia | |
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