Evaluación del flujo geotérmico en manantiales de Aragón
The geothermal flow wich emerges by convection at the springs in Aragon is evaluated, and compared with the theoretical heat flow wich penetrates the surface of the region by conduction. The geological materials through wich the convection takes place are defined (geothermal formations), and the are...
| Autores: | , , , |
|---|---|
| Formato: | artículo |
| Fecha de publicación: | 1999 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9950 |
| Acesso em linha: | http://hdl.handle.net/10272/9950 |
| Access Level: | acceso abierto |
| Palavra-chave: | Geothermal flow Springs Conduction Convection Geothermal formations |
| Resumo: | The geothermal flow wich emerges by convection at the springs in Aragon is evaluated, and compared with the theoretical heat flow wich penetrates the surface of the region by conduction. The geological materials through wich the convection takes place are defined (geothermal formations), and the areas where thermal convection appears most intensely are related |
|---|