Relaciones blastesis deformación del granate en la zona de cizalla de Berzosa
Deformation partitioning is responsible for the various textural and compositional features shown by garnets in the Berzosa Shear Zone. This process is time-and spacedependent across the fault.
| Autores: | , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1987 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/65261 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/65261 |
| Access Level: | acceso abierto |
| Palabra clave: | 552 Ductile shear Deformation partiotioning Garnet Central System Petrología |
| Sumario: | Deformation partitioning is responsible for the various textural and compositional features shown by garnets in the Berzosa Shear Zone. This process is time-and spacedependent across the fault. |
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