{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,10]],"date-time":"2025-10-10T00:51:57Z","timestamp":1760057517602,"version":"build-2065373602"},"reference-count":173,"publisher":"MDPI AG","issue":"2","license":[{"start":{"date-parts":[[2025,2,13]],"date-time":"2025-02-13T00:00:00Z","timestamp":1739404800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"funder":[{"DOI":"10.13039\/501100001871","name":"Funda\u00e7\u00e3o para a Ci\u00eancia e Tecnologia, I.P. (FCT)","doi-asserted-by":"publisher","award":["UI\/BD\/150937\/2021","PRT\/BD\/153588\/2021","UIDB\/04683","SRG 21-46","ALT20-03-0145-FEDER-000028"],"award-info":[{"award-number":["UI\/BD\/150937\/2021","PRT\/BD\/153588\/2021","UIDB\/04683","SRG 21-46","ALT20-03-0145-FEDER-000028"]}],"id":[{"id":"10.13039\/501100001871","id-type":"DOI","asserted-by":"publisher"}]},{"name":"Hugh McKinstry Fund","award":["UI\/BD\/150937\/2021","PRT\/BD\/153588\/2021","UIDB\/04683","SRG 21-46","ALT20-03-0145-FEDER-000028"],"award-info":[{"award-number":["UI\/BD\/150937\/2021","PRT\/BD\/153588\/2021","UIDB\/04683","SRG 21-46","ALT20-03-0145-FEDER-000028"]}]},{"DOI":"10.13039\/501100001871","name":"Alentejo 2020 (Regional Operational Programme of Alentejo) through the FEDER\/FSE\/FEEI","doi-asserted-by":"publisher","award":["UI\/BD\/150937\/2021","PRT\/BD\/153588\/2021","UIDB\/04683","SRG 21-46","ALT20-03-0145-FEDER-000028"],"award-info":[{"award-number":["UI\/BD\/150937\/2021","PRT\/BD\/153588\/2021","UIDB\/04683","SRG 21-46","ALT20-03-0145-FEDER-000028"]}],"id":[{"id":"10.13039\/501100001871","id-type":"DOI","asserted-by":"publisher"}]}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Minerals"],"abstract":"<jats:p>The Ossa-Morena Zone (SW Iberian Massif) hosts the largest set of Cambro\u2013Ordovician 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.<\/jats:p>","DOI":"10.3390\/min15020174","type":"journal-article","created":{"date-parts":[[2025,2,13]],"date-time":"2025-02-13T09:05:42Z","timestamp":1739437542000},"page":"174","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":0,"title":["Ranked Mappable Criteria for Magmatic Units: Systematization of the Ossa-Morena Zone Rift-Related Alkaline Bodies"],"prefix":"10.3390","volume":"15","author":[{"ORCID":"https:\/\/orcid.org\/0000-0003-3643-9122","authenticated-orcid":false,"given":"Jos\u00e9","family":"Roseiro","sequence":"first","affiliation":[{"name":"Departamento de Geoci\u00eancias, Escola de Ci\u00eancias e Tecnologias, Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Ci\u00eancias da Terra (ICT), Polo da Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Investiga\u00e7\u00e3o e Forma\u00e7\u00e3o Avan\u00e7ada, Universidade de \u00c9vora, Pal\u00e1cio do Vimioso, Largo Marqu\u00eas de Marialva, Apart. 94, 7002-554 \u00c9vora, Portugal"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0415-1474","authenticated-orcid":false,"given":"Noel","family":"Moreira","sequence":"additional","affiliation":[{"name":"Departamento de Geoci\u00eancias, Escola de Ci\u00eancias e Tecnologias, Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Ci\u00eancias da Terra (ICT), Polo da Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Investiga\u00e7\u00e3o e Forma\u00e7\u00e3o Avan\u00e7ada, Universidade de \u00c9vora, Pal\u00e1cio do Vimioso, Largo Marqu\u00eas de Marialva, Apart. 94, 7002-554 \u00c9vora, Portugal"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-6338-8845","authenticated-orcid":false,"given":"Daniel","family":"de Oliveira","sequence":"additional","affiliation":[{"name":"Laborat\u00f3rio Nacional de Energia e Geologia, Mineral Resources and Geophysics Research Unit, Estrada da Portela, Bairro do Zambujal, Apt. 7586, Alfragide, 2610-999 Amadora, Portugal"},{"name":"Mineral Resources Expert Group, EuroGeoSurveys, Rue Joseph II, 36-38, P.O. Box 7, 1000 Brussels, Belgium"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6702-5753","authenticated-orcid":false,"given":"Marcelo","family":"Silva","sequence":"additional","affiliation":[{"name":"Departamento de Geoci\u00eancias, Escola de Ci\u00eancias e Tecnologias, Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Ci\u00eancias da Terra (ICT), Polo da Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Investiga\u00e7\u00e3o e Forma\u00e7\u00e3o Avan\u00e7ada, Universidade de \u00c9vora, Pal\u00e1cio do Vimioso, Largo Marqu\u00eas de Marialva, Apart. 94, 7002-554 \u00c9vora, Portugal"}]},{"given":"Luis","family":"Eguiluz","sequence":"additional","affiliation":[{"name":"Departamento de Geodin\u00e1mica, Facultad de Farmacia, Universidad del Pa\u00eds Vasco UPV\/EHU, 01006 Vitoria, Spain"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-6162-0030","authenticated-orcid":false,"given":"Pedro","family":"Nogueira","sequence":"additional","affiliation":[{"name":"Departamento de Geoci\u00eancias, Escola de Ci\u00eancias e Tecnologias, Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"},{"name":"Instituto de Ci\u00eancias da Terra (ICT), Polo da Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7000-761 \u00c9vora, Portugal"}]}],"member":"1968","published-online":{"date-parts":[[2025,2,13]]},"reference":[{"unstructured":"Gillespie, M., Stephenson, D., and Millward, D. 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