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Editorial for the Special Issue “Petrology and Mineralogy of Pegmatite Deposits”

dc.contributor.authorMüller, Axel
dc.contributor.authorRoda Robles, María Encarnación ORCID
dc.date.accessioned2023-09-25T14:55:16Z
dc.date.available2023-09-25T14:55:16Z
dc.date.issued2023-06-15
dc.identifier.citationMinerals 13(6) : (2023) // Article ID 818es_ES
dc.identifier.issn2075-163X
dc.identifier.urihttp://hdl.handle.net/10810/62667
dc.description.abstractThis Special Issue of Minerals, section Mineral Deposits, on the topic of “Petrology and Mineralogy of Pegmatite Deposits”, was inspired by the currently growing scientific and economic interest in pegmatites. Pegmatites are variants of the more common plutonic igneous rocks, such as granites, syenites, and gabbros, which can range from coarse-grained to megacrystic and most frequently occur in rocks of a granitic composition.es_ES
dc.language.isoenges_ES
dc.publisherMDPIes_ES
dc.rightsinfo:eu-repo/semantics/openAccesses_ES
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/
dc.titleEditorial for the Special Issue “Petrology and Mineralogy of Pegmatite Deposits”es_ES
dc.typeinfo:eu-repo/semantics/otheres_ES
dc.date.updated2023-06-27T13:22:21Z
dc.rights.holder© 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).es_ES
dc.relation.publisherversionhttps://www.mdpi.com/2075-163X/13/6/818es_ES
dc.identifier.doi10.3390/min13060818
dc.departamentoesGeología
dc.departamentoeuGeologia


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© 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).
Except where otherwise noted, this item's license is described as © 2023 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/).