Chlorine (Cl) is critical for Earth's habitability and an important tracer for volatile accretion
processes. Yet its chemical behavior during core formation, one of the major events …

We performed experiments to determine the solubility of Au and Pd in magmatic aqueous
fluids as a function of oxygen fugacity (ƒO 2), temperature (T), pH and total chloride …

The spatial association between Pt minerals, magmatic sulfides, and chromite has been
investigated using microbeam X-ray fluorescence (XRF) element mapping and the Maia …

Composition of terrestrial planets records planetary accretion, core–mantle and crust–
mantle differentiation, and surface processes. Here we compare the compositional models …

Halogens are powerful tracers for the accretion of Earth's volatiles. Their sensitivity to Earth's
differentiation, such as core formation, magma ocean crystallization, and planetary …

We present a new analytical method, which allows the simultaneous analysis of fluorine (F),
chlorine (Cl), bromine (Br), and iodine (I) in geological samples. To account for interferences …

The budget of volatile halogens in the bulk silicate Earth, fluorine and chlorine, differs
distinctly from that of chondritic meteorites. Arguably, the bulk silicate Earth shows a low …

Phlogopite and K‐richterite constitute important carrier phases for H and F in Earth's
lithosphere and mantle. The relative importance depends on their stabilities at high pressure …

To assess the viability of sulfide liquid saturation during crystallization of the lunar magma
ocean (LMO), we present a new data set describing both the sulfur (S) concentration at …

This article describes condensation of the elements and use of condensation temperatures
(Tcond) to interpret the volatility trend of the Earth. Major points are:(1) a listing of updated …