Calderas volcánicas pasivas: un ejemplo en el Estefaniense del Pirineo Catalán
A model of volcanic cauldron (pasive volcanic cauldrons) is proposed for some LateHercynian basins of the Catalan Pyrenees. This volcanic structure is defined as a sedimentary basin in which the subsidence processes are accelerated by the volcanic activity triggered by the same tectonic processes wh...
| Autores: | , |
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| Formato: | artículo |
| Fecha de publicación: | 1987 |
| 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:10272/18439 |
| Acesso em linha: | http://hdl.handle.net/10272/18439 |
| Access Level: | acceso abierto |
| Palavra-chave: | Cauldron Ignimbrites Stephanian Pyrenees |
| Resumo: | A model of volcanic cauldron (pasive volcanic cauldrons) is proposed for some LateHercynian basins of the Catalan Pyrenees. This volcanic structure is defined as a sedimentary basin in which the subsidence processes are accelerated by the volcanic activity triggered by the same tectonic processes which are responsible for the basin formation |
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