Un episódio volcánico pre-Cañadas en la Isla de Tenerife
Based on new radiometric data, a Pre-Cañadas volcanic building of 3.5-3.0 Ma has been defined. This new building is mainly compared of basaltic rock cropping out in several gorges to the S of Cañadas Building, inside of the <<Pared de las Cañadas>>, <<Boca d...
| Autores: | , , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1994 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/14014 |
| Acceso en línea: | http://hdl.handle.net/10272/14014 |
| Access Level: | acceso abierto |
| Palabra clave: | Tenerife Canary Islands Cañadas Formation K-Ar geochronology |
| Sumario: | Based on new radiometric data, a Pre-Cañadas volcanic building of 3.5-3.0 Ma has been defined. This new building is mainly compared of basaltic rock cropping out in several gorges to the S of Cañadas Building, inside of the <<Pared de las Cañadas>>, <<Boca de Tauce>>, and <<La Grieta>> and <<La Angostura>> valleys |
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