Earth's carbon, derived from planetesimals in the 1 AU region during accretion of the Solar
System, still retains similarities to carbon found in meteorites (Marty et al. 2013) even after …

Oxygen thermobarometry measurements on spinel peridotite rocks indicate that the oxygen
fugacity at the top of the upper mantle falls within±2 log units of the fayalite-magnetite-quartz …

Exchange between a magma ocean and vapor produced Earth's earliest atmosphere. Its
speciation depends on the oxygen fugacity (f O2) set by the Fe3+/Fe2+ ratio of the magma …

Determining the oxygen fugacity of Earth's silicate mantle is of prime importance because it
affects the speciation and mobility of volatile elements in the interior and has controlled the …

Understanding the origins of the diversity in terrestrial planets is a fundamental goal in Earth
and planetary sciences. In the Solar System, Venus has a similar size and bulk composition …

Micro-analytical determination of Fe 3+/∑ Fe ratios in mid-ocean ridge basalt (MORB)
glasses using micro X-ray absorption near edge structure (μ-XANES) spectroscopy reveals …

Trace-element compositions of olivine from 75 mantle rocks of diverse origin, including
xenoliths from kimberlites, basaltic lavas and orogenic peridotites, were determined by laser …

We document compositions of minerals and melts from 3 GPa partial melting experiments on
two carbonate-bearing natural lherzolite bulk compositions (PERC: MixKLB-1+ 2· 5 wt …

The oxidation state recorded by rocks from the Earth's upper mantle can be calculated from
measurements of the distribution of Fe3+ and Fe2+ between the constituent minerals,,. The …

Geothermobarometric calculations for a worldwide database of inclusions in diamond
indicate that formation of the dominant harzburgitic diamond association occurred …