Plutonismo peralumínico tardihercínico en el sector oriental de Credos (Sistema Central Español): Caracterización y relación con etapas previas
The final stages of late-Hercynian granitoid plutonism in eastern Credos are represented by a series of small issolated peraluminous plutons belonging to the same evolutionary trend than the previous granitic complexes. They are biotite ±muscovite-bearing monzogranites and leucogranites in continuit...
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| Formato: | artículo |
| Fecha de publicación: | 1995 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/13432 |
| Acesso em linha: | http://hdl.handle.net/10272/13432 |
| Access Level: | acceso abierto |
| Palavra-chave: | Peraluminous plutonism Late-Hercynian granitoid Credos |
| Resumo: | The final stages of late-Hercynian granitoid plutonism in eastern Credos are represented by a series of small issolated peraluminous plutons belonging to the same evolutionary trend than the previous granitic complexes. They are biotite ±muscovite-bearing monzogranites and leucogranites in continuity with the differentiation process that gave rise to this hugh granitic province, mainly controlled by fractional crystallization of plagioclase, K-feldspar and minor amounts of biotite and zircon |
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