Palaeomagnetic evidence for non-rotational deformation along the Nea Anchialos Fault System, Central Greece
Four sites in 1.4 Ma old basaltic lavas and two sites in upper Pliocene-lower Quaternary sediments, located both in the hanging-wall and in the footwall blocks of the Nea Anchialos Fault System, have been sampled. This fault system is one of the major E-W trending structures affecting the Thessaly r...
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| Principais autores: | , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Istituto Nazionale di Geofisica e Vulcanologia (INGV)
1997-06-01
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| coleção: | Annals of Geophysics |
| Assuntos: | |
| Acesso em linha: | http://www.annalsofgeophysics.eu/index.php/annals/article/view/3879 |
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