Plutonismo peralumínico tardihercínico en el sector oriental de Credos (Sistema Central Español): Caracterización y relación con etapas previas
Late-Hercynian peraluminous plutonism in eastern Credos (Spanish Central System): Characterization and relationship with previous stages
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Author
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Publication Date
1995 -
Publisher
Sociedad Geológica de España -
Abstract
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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Plutonismo.pdf | 515.2Kb | View/ |
Fichero | Tamaño | Formato |
| Description |
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Plutonismo.pdf | 515.2Kb | View/ |