Primera descripción de capas de esquistos cloríticos con circón en las peridotitas de Ronda (Cordilleras Béticas)
This work reports the finding of layers of zircon-bearing chlorite schists in the southwestern part of the Sierra Bermeja peridotites, the biggest massif of the Ronda peridotites (Alpujarride Complex, Betic Cordillera, southern Spain). Structural, petrographic and geochemical data support a metasoma...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2004 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/8890 |
| Acceso en línea: | http://hdl.handle.net/10272/8890 |
| Access Level: | acceso abierto |
| Palabra clave: | Zr-bearing chlorite schist Serpentinization Rodingitization Ronda peridotites |
| Sumario: | This work reports the finding of layers of zircon-bearing chlorite schists in the southwestern part of the Sierra Bermeja peridotites, the biggest massif of the Ronda peridotites (Alpujarride Complex, Betic Cordillera, southern Spain). Structural, petrographic and geochemical data support a metasomatic origin for these rocks, at temperature conditions of 280-350 ºC, related to the serpentinization of the peridotites and the rodingitization of the granite dykes of the Ronda peridotites |
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