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Estructura de la Cuenca de Ugíjar a partir de datos gravimétricos y magnéticos (Zonas Internas, Cordillera Bética Central) Structure of the Ugíjar Basin using gravity and magnetic data (Internal Zones, Central Betic Cordillera)
| Content Provider | Semantic Scholar |
|---|---|
| Author | Ruiz-Constán, Ana Galindo-Zaldívar, Jesús Andrés-Martínez, Miguel Pedrera, Antonio Martínez-Martos, Manuel |
| Copyright Year | 2013 |
| Abstract | New gravity and magnetic data reveal the geometry and thickness of the Ugijar basin infill and provide additional information about the tectonic structures that deform both the basin and the basement rocks. As previous geological data suggested, the basin is asymmetric and highly conditioned by the activity of ENE-WSW trending faults with right-lateral/normal kinematics that are located in the southern border of the basin. At the northern boundary, the basement top dips smoothly southwards, although there are minor tectonic structures that deform up to the sedimentary infill. Magnetic dipoles have been detected in the northern part of the studied sector, probably associated with small and disperse metallic mineralizations deposited along the Alpujarride/Nevado-Filabride contact. |
| File Format | PDF HTM / HTML |
| Alternate Webpage(s) | http://rabida.uhu.es/dspace/bitstream/handle/10272/7790/Estructura-de-la.pdf;jsessionid=A74B54BCB41F4842C4634F38793A88BD?sequence=2 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |