Both detailed rock magnetism and structural analysis suggest that the routine anisotropy of
magnetic susceptibility (AMS) measurements can not suffice for the interpretations of …

Columnar jointed basalt (CJB) is a kind of jointed rock with a polygonal cylinder mosaic
structure that has complex mechanical properties such as discontinuity and heterogeneity …

Obsidian flow emplacement is a complex and understudied aspect of silicic volcanism. Of
particular importance is the question of how highly viscous magma can lose sufficient gas in …

The strength behavior and deformation modulus of columnar jointed rock mass have been
investigated by conducting a series of uniaxial compressive tests, along with consideration …

Solidification, emplacement and fluid dynamics of a sub-volcanic rock at Mt Etna have been
investigated through two-dimensional (2D) and three-dimensional (3D) textural analyses of …

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 …

Magnetic fabrics were investigated in the sub-volcanic bodies occurring within the SW
Flysch Belt of the Western Carpathians. Magnetite or low-Ti titanomagnetite is the principal …

Abstract This Special Publication provides a snapshot of our understanding of volcanic
processes through the use of palaeomagnetic and rock magnetic techniques. Here, we …

Anisotropy of magnetic susceptibility (AMS) and anisotropy of magnetic remanence (AARM
and AIRM) are efficient and versatile techniques to indirectly determine rock fabrics. Yet …

Lava has complex geochemical characteristics based on differences in eruption centers,
eruptive events, and flow emplacement. Characterization of lava is useful for understanding …