Unraveling magnetic fabrics

The anisotropy of magnetic susceptibility has been proven to be an excellent indicator for mineral fabrics and therefore deformation in a rock or sediment. Low-field anisotropy is relatively rapid to measure so that a sufficient number of samples can be measured to obtain a good statistical represen...

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Bibliographic Details
Published in:International Journal of Earth Sciences : GR Geologische Rundschau, Vol. 101, No. 3 (2012), p. 613-624
Main Author: Hirt, M.
Other Involved Persons: Almqvist, G.
Format: electronic Article
Physical Description:Online-Ressource
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