In the past couple of decades, the laser-heated diamond anvil cell (combined with in situ
techniques) has become an extensively used tool for studying pressure-temperature …

The terrestrial planets accreted from a diverse suite of solar system materials ranging from
strongly O-deficient materials similar to enstatite chondrites via ordinary chondrite materials …

We provide experimental and theoretical evidence for a pressure-induced Mott insulator-
metal transition in Fe 2 O 3 characterized by site-selective delocalization of the electrons …

Deciphering the origin of seismic velocity heterogeneities in the mantle is crucial to
understanding internal structures and processes at work in the Earth. The spin crossover in …

Iron oxides are fundamentally important compounds for basic and applied sciences as well
as in numerous industrial applications. In this work we report the synthesis and investigation …

Complex seismic, thermal, and chemical features have been reported in Earth's lowermost
mantle. In particular, possible iron enrichments in the large low shear‐wave velocity …

We present local density approximation augmented by the Hubbard‐type correction
calculations of high‐temperature elastic properties of bridgmanite with composition for …

SYNCmoss is a software package dedicated to fitting Mössbauer spectra measured with a
synchrotron Mössbauer source (SMS). Operation conditions of an SMS can be continuously …

The accurate determination of melting curves for transition metals is an intense topic within
high pressure research, both because of the technical challenges included as well as the …

Heterogeneity in Earth's mantle is a record of chemical and dynamic processes over Earth's
history. The geophysical signatures of heterogeneity can only be interpreted with …