Anisotropy of magnetic susceptibility (AMS) and anisotropy remanence (AARM AIRM) are efficient versatile techniques to indirectly determine rock fabrics. Yet, deciphering the source a fabric remains crucial challenging step, notably in presence ferrimagnetic phases. Here we use X-ray micro-computed tomography directly compare mineral shape-preferred orientation spatial distribution fabrics AMS,...

The study of basaltic samples returned half a century ago through the Apollo missions has provided unparalleled insights into magmatic processes associated with volcanism on planetary bodies. Traditional these been conducted in two dimensions (2D) via interrogation thin sections and subsequent in-situ chemical analyses, yet are three-dimensional (3D) objects therefore preserve evidence lunar vo...

Seismic anisotropy produced by aligned olivine in oceanic lithosphere offers a window into mid-ocean ridge (MOR) dynamics. Yet, interpreting the context of grain-scale deformation processes and strain observed laboratory experiments natural samples has proven challenging due to incomplete seismological constraints length scale differences spanning orders magnitude. To bridge this observational ...