Water in Earth's deep interior is predicted to be hydroxyl (OH−) stored in nominally
anhydrous minerals, profoundly modulating both structure and dynamics of Earth's mantle …

Earth's inner core (IC) is less dense than pure iron, indicating the existence of light elements
within it. Silicon, sulfur, carbon, oxygen and hydrogen have been suggested to be the …

Understanding high-pressure-stimulated circularly polarized luminescence (CPL) of
enantiomers remains a challenging but significant task in fundamental research and optical …

Large igneous province volcanism represents extensive mantle melting that has contributed
to Earth's chemical differentiation and lithospheric and climatic changes. Compositional …

The origin of water on the Earth is a long-standing mystery, requiring a comprehensive
search for hydrous compounds, stable at conditions of the deep Earth and made of Earth …

Hydrogen, the most abundant element in the universe, has likely been incorporated into
Earth's core due to its tendency to dissolve in iron at high pressure. Using machine-learning …

The elements hydrogen, carbon, nitrogen and oxygen are assumed to comprise the bulk of
the interiors of the ice giant planets Uranus, Neptune, and sub-Neptune exoplanets. The …

Hydrous and nominally anhydrous minerals are a fundamental class of solids of enormous
significance to geophysics. They are the water carriers in the deep geological water cycle …

High-pressure structural, vibrational, and electrical transport properties of CrCl3 were
investigated by means of Raman spectroscopy, electrical conductivity, and high-resolution …

Seismological observations suggest that Earth's inner core (IC) is heterogeneous and
anisotropic. Increasing seismological observations make the understanding of the …