Anisotropy of magnetic susceptibility (AMS) was recognized as a feature of minerals in 1899,
and petrofabric-compatible AMS fabrics were reported from 1942–1958. Shortly thereafter …

Magnetic fabric (MF) investigations complemented by geochemical and grain surface
analyses of the understudied and controversial marine isotope stage (MIS) 5 b, 4 and 3 …

For 40 years magnetic anisotropy has provided successful geological interpretations of
magnetic ellipsoid orientations; in contrast the interpretation of anisotropy magnitudes is far …

Statistics of Earth Science Data: Their Distribution in Time, Space and Orientation |
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The anisotropy of magnetic susceptibility (AMS) of single crystals of biotite, muscovite and
chlorite has been measured in order to provide accurate values of the magnetic anisotropy …

The magnetic anisotropy of rocks results from the contributions of diamagnetic,
paramagnetic, and ferromagnetic (in the broad sense) minerals. This bulk anisotropy of …

Empirical relationships between magnetic fabrics and deformation have long served as a
fast and efficient way to interpret rock textures. Understanding the single crystal magnetic …

Abstract The Anisotropy of Magnetic Susceptibility (AMS) is a well-established petrofabric
tool for indicating relative strain and microstructural character and has been validated on …

Magmatic sill intrusions develop saucer‐like geometries in layered sedimentary basins
intruded by large volumes of magma. Saucer‐shaped sill emplacement models are based …

The Itapetim pluton is a sigmoid-shaped intrusion bounded by the NE-SW, sinistral Itapetim
and Taperoá shear zones. The Anisotropy of Magnetic Susceptibility (AMS) and Anhysteretic …