Development of the AMS method for unconsolidated sediments. Application to tsunami deposits
AMS (Anisotropy of Magnetic Susceptibility) is a geophysical method, which uses the electromagnetic properties of samples as a proxy of their fabric. Commonly used on hard rocks and cohesive sediments, the method has never been developed for unconsolidated sediments before. In this contribution, we...
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| Autori principali: | , |
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| Natura: | Artigo |
| Lingua: | Inglês |
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Groupe français de géomorphologie
2011
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| Soggetti: | |
| Accesso online: | https://doi.org/10.4000/geomorphologie.9491 https://hdl.handle.net/20.500.13089/gip3 https://journals.openedition.org/geomorphologie/9491 |
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