The Hercynian granitic rocks of the North-Eastern Iberian Peninsula.
Most of Pyrenean and Calalonian Coastal Ranges granitoids show typical calc-alkaline trends and Peacock indexes of such series remain at high values. This fact marks an evident difference between these granitoids and those from other hercynian massifs (e.g. Iberian Massif). Such values are typical f...
| Autores: | , , |
|---|---|
| Formato: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1988 |
| País: | España |
| Recursos: | Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| Repositorio: | Recercat. Dipósit de la Recerca de Catalunya |
| OAI Identifier: | oai:recercat.cat:2445/99285 |
| Acesso em linha: | https://hdl.handle.net/2445/99285 |
| Access Level: | acceso abierto |
| Palavra-chave: | Petrologia Granit Península Ibèrica Petrology Granite Iberian Peninsula |
| Resumo: | Most of Pyrenean and Calalonian Coastal Ranges granitoids show typical calc-alkaline trends and Peacock indexes of such series remain at high values. This fact marks an evident difference between these granitoids and those from other hercynian massifs (e.g. Iberian Massif). Such values are typical features of plutonic rocks formed in compressive plate magins. |
|---|