Abstract A 3D rotator (for MFK1-FA or MFK1-A Kappabridges) was developed to increase
the speed and comfort of anisotropy of magnetic susceptibility (AMS) measurements. The 3D …

Magnetic pore fabrics (MPF) are an efficient way to characterize pore space anisotropy, ie,
the average pore shape and orientation. They are determined by impregnating rocks with …

Feldspars are the most abundant rock-forming minerals in the Earth's crust, but their
magnetic properties have not been rigorously studied. This work focuses on the intrinsic …

The anisotropy of magnetic susceptibility of ferrofluid‐impregnated samples is an efficient
and powerful proxy for pore space anisotropy and preferred flow directions. One of the main …

Anisotropy of magnetic susceptibility (AMS) is often used as a proxy for mineral fabric in
deformed rocks. To do so quantitatively, it is necessary to quantify the intrinsic magnetic …

Anisotropy of magnetic susceptibility is a petrofabric tool used to estimate the alignment of
minerals at the site-scale, the imbrication between the magnetic foliation and the …

Magnetic fabrics are used extensively as proxies for mineral fabrics and to correct
paleomagnetic data, and have been proposed to quantify pore fabrics. Today's …

The magnetic anisotropy exhibited by ferrofluid-impregnated samples serves as a proxy for
their pore fabrics, and is therefore known as magnetic pore fabric (MPF). Empirically, the …

Pyroxenes constitute an important component in mafic igneous and metamorphic rocks.
They often possess a prismatic habit, and their long axis, the crystallographic c axis, helps …

Mantle flow dynamics can cause preferential alignment of olivine crystals that results in
anisotropy of physical properties. To interpret anisotropy in mantle rocks, it is necessary to …