The application of Mo isotopes to study geodynamic processes is a rather new development
that has gained considerable momentum over the past few years. Its redox-sensitivity …

The halogens (F, Cl, Br, I) form an important suite of tracers of igneous processes, and may
be used to track magmas from their point of origin, through their differentiation, evolution …

The zinc stable isotope system has been successfully applied to many and varied fields in
geochemistry, but to date it is still not completely clear how this isotope system is affected by …

In this study potential iron isotope fractionation by magmatic processes in the Earth's crust
was systematically investigated. High precision iron isotope analyses by MC-ICP-MS were …

Iceland is one of the most active and productive terrestrial volcanic regions, with eruption
frequency of≥ 20 events per century and magma output rates of≥ 5 km3 per century …

Eruptive column models are powerful tools for investigating the transport of volcanic gas and
ash, reconstructing past explosive eruptions, and simulating future hazards. However, the …

The Si isotopic composition of Earth's mantle is thought to be homogeneous (δ30Si=−
0.29±0.08‰, 2s. d.) and not greatly affected by partial melting and recycling. Previous …

Indirect evidence for the presence of a felsic continental crust, such as the elevated
49Ti/47Ti ratios in Archean shales, has been used to argue for ongoing subduction at that …

Water and carbon dioxide are the most abundant volatile components in terrestrial magmas.
As they exsolve into magmatic vapour, they promote magma buoyancy, accelerating ascent …

As volatile and variably mobile components, halogens play key roles in magmatic,
metasomatic, mineralizing, and volcanic processes by influencing the physical and chemical …