The deployment of seismic stations and the development of ambient noise tomography as
well as new analysis methods provide an opportunity for higher-resolution imaging of …

Olivine, a ferromagnesian orthosilicate, is the most abundant mineral in Earth's upper mantle
and is stable down to the olivine–wadsleyite phase transition, which defines the 410 km …

We present constraints on the hydration state and rheology of the lithospheric mantle
beneath the North Anatolian fault zone (NAFZ). Peridotite xenoliths from the Biyikali and …

The podiform chromitite found within the Luobusha ophiolite comprises characteristic
nodules and massive chromitites. However, the exact origin of these formations remains a …

Many minerals within the subcontinental lithospheric mantle (SCLM) contain structurally
bonded hydrogen (commonly referred to as 'water'), which significantly impacts their …

Seismic anisotropy produced by aligned olivine in oceanic lithosphere offers a window into
mid‐ocean ridge (MOR) dynamics. Yet, interpreting anisotropy in the context of grain‐scale …

We characterize and quantify the microstructure, hydrogen concentrations, and seismic
properties of a tectonically exhumed sliver of oceanic lithospheric mantle outcropping in the …

We report on the petrology, microstructure and seismic properties of 44 peridotite xenoliths
extracted from the upper mantle beneath Marie Byrd Land (MBL), West Antarctica. The aim …

The microstructural relationship between olivine and clinopyroxene is significant in
recovering the mantle evolution under clinopyroxene-saturated melting conditions. This …

Predicting the incorporation of hydrogen (H) in the atomic structure of upper mantle minerals
is a major target in geodynamics since hydration impacts essential physico-chemical …