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A palaeomagnetic study of Upper Pliocene volcanic rocks in the area of the Levant Fault near Homs, western Syria
Thermal demagnetisation of samples from 75 sites in basaltic rocks, mostly within 5 km of the Levant Fault, identifiesconsistent directions of remanence in most sites. Normal, Reversed and Intermediate polarities are identified, with Reversedpolarities dominating. The Normal and Reversed sites are s...
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| Publicado no: | Geofísica Internacional |
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| Main Authors: | , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Universidad Nacional Autónoma de México
2005
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| Assuntos: | |
| Acesso em linha: | https://www.redalyc.org/articulo.oa?id=56844301 |
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