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Estructura de la cuenca sedimentaria de Tabernas-Sorbas mediante prospección gravimétrica y magnética (Zonas Internas, Cordillera Bética Oriental) Structure of the Tabernas-Sorbas sedimentary basin by gravity and magnetic survey (Internal Zones, Eastern Betic Cordillera)
| Content Provider | Semantic Scholar |
|---|---|
| Author | Li, Qiao Ruano, Patricia Pedrera, Antonio Galindo-Zaldívar, Jesús |
| Copyright Year | 2012 |
| Abstract | Gravity and total field magnetic anomaly data were obtained across three profiles in the Tabernas-Sorbas basin (Internal Zones, Eastern Betics). Gravity models show an asymmetric basin shape with the thicker sedimentary sequences close or attached to its southern edge. A magnetic dipole, located in the northern half of the profiles, is associated to ore bodies in the basement, linked to the Alpujarride / Nevado-Filabride contact. The basin evolution was controlled by the development of an E-W to ENE-WSW synform and the activity of E-W to ESE-WNW dextral-reverse faults in its southern boundary. |
| File Format | PDF HTM / HTML |
| Alternate Webpage(s) | http://sociedadgeologica.es/archivos/geogacetas/geo52/art29.pdf |
| Alternate Webpage(s) | http://rabida.uhu.es/dspace/bitstream/handle/10272/7233/Estructura-de-la-cuenca.pdf?sequence=2 |
| Language | English |
| Access Restriction | Open |
| Content Type | Text |
| Resource Type | Article |