Penetrating, high-energy synchrotron X-rays are in strong demand, particularly for high-
pressure research in physics, chemistry and geosciences, and for materials engineering …

A high‐magnetic field once existed in the early history of the Moon, suggesting the core
once possessed a thermally driven dynamo. The thermal conductivity of core materials is a …

Paleomagnetic analyses have suggested that the lunar magnetic field underwent a
significant change from 4.25 to 3.19 Ga, indicating the rapid transition of the lunar dynamo …

Abstract Dense Fe‐Ti‐rich cumulates, formed as the last dregs of the lunar magma ocean,
are thought to have driven a large‐scale overturn of the lunar mantle over 4 Ga ago …

Deeply subducted carbonates likely cause low-degree melting of the upper mantle and thus
play an important role in the deep carbon cycle. However, direct seismic detection of …

Iron-rich silicate melts play an important role in the magmatic history of the Earth and the
Moon. However, their elastic properties at high pressures, especially the sound velocities …

Sound velocity and equation of state of liquids provide important constraints on the
generation, presence, and transport of silicate and metallic melts in the Earth's interior …

Based on cosmochemistry evidence and element partitioning experiments, phosphorus is
thought to be present in the iron‐rich cores of Earth and Moon. Phosphorus has a similar …

Sound velocities of diopside liquid were determined at high pressures and temperatures up
to 3.8 GPa and 2375 K, using the ultrasonic technique combined with synchrotron X‐ray …

Subduction of carbonate‐bearing oceanic plates into Earth's interior recycles carbon from
the surface to the deep mantle. The subducted carbonates can significantly affect mantle …