Magnetic anomalies associated to extensional detachments? An example at Xistral TectonicWindow of the Lugo Dome (NW Spain)
[EN]Magnetic anomalies in the Lugo gneiss dome of the NW Iberian Massif are related with outcropping late Variscan extensional detachments The sources of magnetic anomalies are high‐grade metamorphic rocks, including migmatites and inhomogeneous granites The Lugo Dome is one of a series that coincid...
| Autores: | , , , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2018 |
| País: | España |
| Institución: | Universidad de Salamanca (USAL) |
| Repositorio: | GREDOS. Repositorio Institucional de la Universidad de Salamanca |
| OAI Identifier: | oai:gredos.usal.es:10366/138846 |
| Acceso en línea: | http://hdl.handle.net/10366/138846 |
| Access Level: | acceso abierto |
| Palabra clave: | Solid earth physics Magnetism Extensional Detachments Lugo-Sanabria Extensional Dome Central Iberian Zone |
| Sumario: | [EN]Magnetic anomalies in the Lugo gneiss dome of the NW Iberian Massif are related with outcropping late Variscan extensional detachments The sources of magnetic anomalies are high‐grade metamorphic rocks, including migmatites and inhomogeneous granites The Lugo Dome is one of a series that coincides with a broad, curved magnetic anomaly that delineates an orocline in NW Iberia |
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