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 …

When studying weakly anisotropic rocks non-standard relationships between magnetic and
expected petrofabric axes are sometimes observed, in particular the so-called inverse or …

We report on the anisotropy of magnetic susceptibility (AMS) analyses of fine-grained
sediments deposited during the Messinian in foredeep basins at the front of the northern …

A mixed-polarity zone, representing alternations between remagnetized and non-
remagnetized strata, has been documented within the lower few metres of the CRP-1 core …

Although the tectonic features and stress regime typical for accretionary complexes and
back-arc domains have been widely documented so far, few are known on the transitional …

The Teplá–Barrandian unit (TBU) of Central Europe's Bohemian Massif exposes perhaps
the best preserved fragment of an accretionary wedge in the Avalonian–Cadomian belt …

Inverse magnetic fabrics defined by anisotropy of magnetic susceptibility with the longest
principal axis perpendicular to bedding were identified in the studied samples of Ordovician …

Anisotropy of magnetic remanence (AMR) is increasingly being applied to palaeomagnetic
and structural fabric studies. AMR techniques measure the anisotropy of the remanence …

New detrital zircon-fission track (ZFT) and magnetic fabric data are presented to constrain
the time of deposition, provenance and deformation of the of Lower and Upper members of …

A 28-m-long section situated on the coast of the Arctic Ocean, Russia (74° N, 113° E) was
extensively sampled primarily for the purpose of magnetostratigraphic investigations across …