High pressure mineral assemblages in the Trevenque Unit (Central Alpujarrides, Andalucía)
The Trevenque Unit is located in the Alpujarride Complex. In this unit, the Fe-Mg carpholite, cloritoid, chlorite, kyanite aragonite assemblages show metamorphic evolution at HP-LT conditions The metamorphic peal< is estimated to have been at 400-4500 C and at least 10 Kb. The pressure condit...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1991 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | inglés |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/17988 |
| Acceso en línea: | http://hdl.handle.net/10272/17988 |
| Access Level: | acceso abierto |
| Palabra clave: | Alpujárride Complex High pressure metamorphism Fe-Mg carpholite |
| Sumario: | The Trevenque Unit is located in the Alpujarride Complex. In this unit, the Fe-Mg carpholite, cloritoid, chlorite, kyanite aragonite assemblages show metamorphic evolution at HP-LT conditions The metamorphic peal< is estimated to have been at 400-4500 C and at least 10 Kb. The pressure conditions in the Alpujarride Complex are similar to those observed in the underlying Nevado-Filabrides Complex |
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