First estimations of terrestrial heat flow in the TMVB and adjacent areas based on isotopic composition of natural helium
The Transmexican Volcanic Belt is the most active zone of recent volcanism in Southern Mexico. However, only a few heat tlow data have been collected In the region. In the present work a non-traditional approach Is used to calculate tt.rrestrial heat tlow by means of the 3He/4He ratio in gases of ge...
| Autores: | , , , , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 1985 |
| País: | México |
| Institución: | UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO |
| Repositorio: | Geofísica Internacional |
| Idioma: | español |
| OAI Identifier: | oai:revistagi.geofisica.unam.mx:article/1028 |
| Acceso en línea: | http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/1028 |
| Access Level: | acceso abierto |
| Palabra clave: | Vulcanismo Flujo Calor terrestre TMVB Composición isotópica Helio natural Volcanism Flow Terrestrial heat Isotopic composition Natural helium Cinturón Volcánico Mexicano |
| Sumario: | The Transmexican Volcanic Belt is the most active zone of recent volcanism in Southern Mexico. However, only a few heat tlow data have been collected In the region. In the present work a non-traditional approach Is used to calculate tt.rrestrial heat tlow by means of the 3He/4He ratio in gases of geothennal origin. The data obtained delineate the main volcanic systems of the Belt and its limits. |
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