Gravimetric study of Lanzarote Island
A gravimetric survey of the volcanic island of Lanzarote (Canary Islands) is presented. The date are studied, determining two anomalies component waves by means of least square prediction. The final anomalies model is considered to obtain information about the inner mass density distribution, reprod...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1990 |
| País: | España |
| Recursos: | Consejo Superior de Investigaciones Científicas (CSIC) |
| Repositorio: | DIGITAL.CSIC. Repositorio Institucional del CSIC |
| OAI Identifier: | oai:digital.csic.es:10261/24403 |
| Acesso em linha: | http://hdl.handle.net/10261/24403 |
| Access Level: | acceso abierto |
| Palavra-chave: | Gravimetría Volcanismo Geodinámica Lanzarote |
| Resumo: | A gravimetric survey of the volcanic island of Lanzarote (Canary Islands) is presented. The date are studied, determining two anomalies component waves by means of least square prediction. The final anomalies model is considered to obtain information about the inner mass density distribution, reproducing the underground perturbations as spherical bodies. Dificulties of regional trend definition are found, nevertheless several conclusions about the mass distribution are pointed. |
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