Melt inclusions in phenocrysts are a potentially powerful tool in petrological research that
can provide the only direct information available on the physical parameters (P, T and melt …

The equations for the chemical potentials of fayalite and forsterite components in olivine and
liquid may be used to derive a thermodynamic expression for the exchange coefficient K^\;\; …

Crystallization experiments were performed at 200 MPa in the temperature range 1150–
950° C at oxygen fugacities corresponding to the quartz–fayalite–magnetite (QFM) and MnO …

To investigate the effect of water on phase relations and compositions in a basaltic system,
we performed crystallization experiments at pressures of 100, 200 and 500 MPa in a …

The purpose of this review study is to reappraise in a more comprehensive form the
thermodynamic principles behind the partitioning of trace elements between clinopyroxene …

Both scaled laboratory experiments and numerical models of terrestrial mantle plumes
produce 'balloon-on-a-string'structures, with a bulbous head followed by a stem-like tail …

High-precision electron microprobe analyses were obtained on olivine grains from
Klyuchevskoy, Shiveluch and Gorely volcanoes in the Kamchatka Arc; Irazú, Platanar and …

Lattice diffusion coefficients have been determined for 19 elements (Li, Be, Na, Ca, Sc, Ti, V,
Cr, Mn, Fe, Co, Ni, Zn, Y, Zr, Eu, Gd, Lu and Hf) in a single crystal of San Carlos olivine as a …

Understanding magmatic processes such as crystallization and melting recorded in natural
samples requires calibration of mineral–melt trace element partition coefficients (D) and their …

Abstract China's Chang'E-5 mission returned new samples from the Moon and has extended
the eruption ages of lunar volcanism ca. 800 million years younger than previous …