Secuencia magnetoestratigráfica y edad de los materiales volcánicos y sedimentarios de Poblete (Ciudad Real)
The magnetostratigraphic sequence of the volcanosedimentary materials near to Poblete (Ciudad Real) has allowed dating the most recent eruption of the volcanism of the Campo de Calatrava. The chronology of the magnetostratigraphic sequence has based on the radiometric dating of one lava flow that wa...
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2002 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/9379 |
| Acceso en línea: | http://hdl.handle.net/10272/9379 |
| Access Level: | acceso abierto |
| Palabra clave: | Paleomagnetism Magnetostratigraphy Phreatomagmatic volcanism Radiometric ages Campo de Calatrava |
| Sumario: | The magnetostratigraphic sequence of the volcanosedimentary materials near to Poblete (Ciudad Real) has allowed dating the most recent eruption of the volcanism of the Campo de Calatrava. The chronology of the magnetostratigraphic sequence has based on the radiometric dating of one lava flow that was previous to the explosive episodes. A great variety of volcanic materials and several sedimentary levels and soils compose the sequence |
|---|