Using the anisotropy of magnetic susceptibility to infer flow-induced orientation of anisotropic particles: feasibility and sensitivity

Author:

Akkoyun Meral,Majesté Jean-Charles,Bascou Jérome

Publisher

Springer Science and Business Media LLC

Subject

Condensed Matter Physics,General Materials Science

Reference26 articles.

1. Arbaret L, Fernandez A, Jezek J, Ildefonse B, Launeau P, Diot H (2000) Analogue and numerical modelling of shape fabrics: consequences for strain and flow determination in magmas. Trans R Soc Edinb Earth Sci 90:97–109

2. Bascou J, Camps P, Dautria JM (2005) Magnetic versus crystallographic fabrics in a basaltic lava flow. J Volcanol Geotherm Res 145:119–135

3. Bay RS, Tucker CL (1992) Fiber orientation in simple injection moldings. Part I: theory and numerical methods. Polym Compos 13:317–331

4. Bouchez JL (1997) Granite is never isotropic: an introduction to AMS studies of granitic rocks. In: Granite: from segregation of melt to emplacement fabrics. Kluwer Acad. Publ., pp 95–112

5. Cañón-Tapia E, Chávez-Álvarez M (2004) Theoretical aspects of particle movement in flowing magma: implication for the anisotropy of magnetic susceptibility of dykes and lava flows. In: Magnetic fabric methods and applications. Geological Society, London, Special Publications, London, pp 227–249

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