La Maladeta and Bono granites at depth from geophysical data (Central Pyrenees)
This work aims to show a compilation of geophysical data (gravity, magnetic and magnetotelluric data) to determine the upper crustal structure and geometry at depth of the La Maladeta and Bono granites (Central Pyrenees). La Maladeta granite is interpreted as an asymmetric granitic complex 8 km-thic...
| Autores: | , , , , , , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2025 |
| 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:10272/27144 |
| Acceso en línea: | https://hdl.handle.net/10272/27144 |
| Access Level: | acceso abierto |
| Palabra clave: | La Maladeta granite Bono granite Gravity Magnetotellurics Magnetic anomalies Granito La Maladeta Granito de Bono Gravimetría Prospección magnetotelúrica Anomalías magnéticas 2506 Geología |
| Sumario: | This work aims to show a compilation of geophysical data (gravity, magnetic and magnetotelluric data) to determine the upper crustal structure and geometry at depth of the La Maladeta and Bono granites (Central Pyrenees). La Maladeta granite is interpreted as an asymmetric granitic complex 8 km-thick formed by two differentiated bodies and with a clearly northwards deepening. By contrast, the Bono granite shows a laminar geometry and its thickness does not reach 1.5 km. Both granites show higher areal extension at depth than that showed by their outcrops at surface. --------------------------------------------------------------------------------------------------------- |
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