Estudio microgravimétrico en la Caldera del Teide
In this study, the first results obtained in a gravimetric exploration in the Caldera of Teide, Tenerife, Canary Islands, are presented. The gravimetric anomalies observed permit us to deduce the existence of a double vault, with an important mass deficit centered in the southeast base of the volcan...
| Authors: | , , |
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| Format: | book |
| Publication Date: | 1986 |
| Country: | España |
| Institution: | Universidad Complutense de Madrid (UCM) |
| Repository: | Docta Complutense |
| Language: | Spanish |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/65548 |
| Online Access: | https://hdl.handle.net/20.500.14352/65548 |
| Access Level: | Open access |
| Keyword: | 528 Geodesia Volcanología Geodesy Volcanology Gravimetría Gravimetry Geodinámica Geodynamics Crustal movements Deformación Tenerife Teide 2504 Geodesia |
| Summary: | In this study, the first results obtained in a gravimetric exploration in the Caldera of Teide, Tenerife, Canary Islands, are presented. The gravimetric anomalies observed permit us to deduce the existence of a double vault, with an important mass deficit centered in the southeast base of the volcano Teide that seems to support the hypothesis of a caldera collapse, at least for an important part of the present depression. |
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