Consideraciones sobre la rubefacción de algunos granitos ibéricos.
[ENG]Red granites are regarded as products of metasomatism by alkaline aqueous fluids (PH2O above 1-2 Kb)not derived from acid magma, but deep levels.
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| Main Authors: | , |
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| Format: | artículo biblioteca |
| Language: | Spanish / Castilian |
| Published: |
CSIC - Instituto de Ciencias de la Tierra Jaume Almera (ICTJA)
1979
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| Subjects: | Rubefacción, Granitos ibéricos, |
| Online Access: | http://hdl.handle.net/10261/31020 |
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| Summary: | [ENG]Red granites are regarded as products of metasomatism by alkaline aqueous fluids (PH2O above 1-2 Kb)not derived from acid magma, but deep levels. |
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