dc.contributor.author | Andonaegui, P. | |
dc.date.accessioned | 2020-05-14T10:56:02Z | |
dc.date.available | 2020-05-14T10:56:02Z | |
dc.date.issued | 1991 | |
dc.identifier.uri | http://hdl.handle.net/10272/17951 | |
dc.description.abstract | In the plutonic complex of Mora-Gálvez (south Toledo) we have distinguished three types of granitoids: coarse grained granites, porphiritc granites and cordierite nodules leucogranites. Al/ of them are biotite-bearing and they usually have minor cordierite. Geochemically are peralouminous and their origin could be from melting of crustal rocks | es_ES |
dc.language.iso | spa | es_ES |
dc.publisher | Sociedad Geológica de España | es_ES |
dc.rights | Atribución-NoComercial-SinDerivadas 3.0 España | * |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/3.0/es/ | * |
dc.subject.other | Geochemistry | es_ES |
dc.subject.other | Peralouminous granites | es_ES |
dc.subject.other | Iberian Hercynian belt | es_ES |
dc.title | Caracterización geoquímica de los granitoides de Mora Gálvez (Toledo) | es_ES |
dc.type | info:eu-repo/semantics/article | es_ES |
dc.rights.accessRights | info:eu-repo/semantics/openAccess | es_ES |