The hydration and complexation of metals in hydrothermal fluids are key processes
controlling the mobility of elements in the Earth's crust, leading to the formation of ore …

The effect of fluorine on the solubilities of Mn-columbite (MnNb 2 O 6), Mn-tantalite (MnTa 2
O 6), zircon (ZrSiO 4) and hafnon (HfSiO 4) were determined in highly fluxed, water …

Halogens, mainly F and Cl, play key roles in the evolution and rheology of silicic magmas,
magmatic-hydrothermal transition, partitioning of metals into aqueous fluids, and formation …

The characteristic REE fractionation pattern in arc magmas compared to MOR-basalts
results from the selective mobilization of light rare-earth elements (LREE) by slab-derived …

Abstract Biotite–melt Nb and Ta partition coefficients (DNb and DTa) are crucial for
understanding Nb− Ta enrichment and fractionation in rare metal granites (RMGs) …

Lithium‐rich disordered rock‐salt oxides have attracted great interest owing to their
promising performance as Li‐ion battery cathodes. While experimental and theoretical …

The effect of F and Cl on trace element recycling during subduction-related sediment melting
has been investigated by performing piston-cylinder experiments with a hydrous …

Ore minerals of niobium and tantalum are typically associated with pegmatites and rare
metal granites; these include columbite, tantalite, wodginite, titanowodginite, microlite and …

Fluids1 in subduction zones have been a subject of growing interest for at least the last 20
years. Subduction zones are the major places on Earth for mass transfer, element recycling …

Br speciation in hydrous silicate melts at high pressure has been investigated up to 7.6 GPa
using X-ray absorption spectroscopy (XAS) at the Br K-edge in a Paris–Edinburgh press. Br …