Los granates del tramo del núcleo de la Sierra de los Santos (Córdoba)
The Sierra de los Santos (Sierra Morena, prov. of Córdoba) consists of precambric and paleozoic materials, essentially chloritic schists, limestones and small outcrops of acid and basic igneous rocks. The garnets studied in this work are the only relict minerals from the first metamorphism process d...
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1983 |
| País: | España |
| Institución: | Universidad de Murcia |
| Repositorio: | DIGITUM. Depósito Digital Institucional de la Universidad de Murcia |
| OAI Identifier: | oai:digitum.um.es:10201/5671 |
| Acceso en línea: | http://hdl.handle.net/10201/5671 |
| Access Level: | acceso abierto |
| Palabra clave: | Geología CDU::5 - Ciencias puras y naturales::55 - Geología. Meteorología |
| Sumario: | The Sierra de los Santos (Sierra Morena, prov. of Córdoba) consists of precambric and paleozoic materials, essentially chloritic schists, limestones and small outcrops of acid and basic igneous rocks. The garnets studied in this work are the only relict minerals from the first metamorphism process developped in this área. X-ray, optical and chemical data of these garnets are reported. They correspond to the piralspite series; finally, metamorphism conditions having given birth to the garnets are discussed. |
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