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 …

The use of the Anisotropy of Magnetic Susceptibility (AMS) has become a rather common
practice in Earth Sciences since the pioneer note by Graham. The versatility of the …

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

Magnetostratigraphy of 222 remanent directions together with late Oligocene to early
Miocene mammal and charophyte paleontology suggest that 2179 m of the Xishuigou …

Magnetic lineation in rocks is given by a cluster of the principal axes of maximum
susceptibility (Kmax) of the Anisotropy of Magnetic Susceptibility (AMS) tensor. In deformed …

Reconstructing the deformation sequence and strain history of the Longmen Shan thrust belt
(LSTB) has significant implications for the growths of the SW Qinling orogenic belt and the …

Abstract The Tibetan Plateau accommodated major upper crustal shortening during Indian
Plate oceanic and continental lithosphere subduction. Deciphering whether shortening was …

A new paleomagnetic pole position is obtained from the well-dated (636.3±4.9 Ma) Nantuo
Formation in the Guzhang section, western Hunan Province, and the correlative Long'e …

For over thirty years the anisotropy of magnetic susceptibility (AMS) has been exploited in
rock fabric studies. Our knowledge of the mechanisms leading to magnetic fabric …

The timing of onset of deposition of the Lulehe Formation is a significant factor in
understanding the genesis of the Qaidam basin and the evolution of the Tibetan Plateau …