Earth is unique among the terrestrial planets in our solar system in having a fluid envelope
that fosters life. The secrets behind Earth's habitable climate are well-tuned cycles of carbon …

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

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 …

Kimberlite and carbonatite magmas that intrude cratonic lithosphere are among the deepest
probes of the terrestrial carbon cycle. Their co-existence on thick continental shields is …

Subduction tectonics imposes an important role in the evolution of the interior of the Earth
and its global carbon cycle; however, the mechanism of the mantle–slab interaction remains …

We report new data on the geochemical evolution, metasomatic and deformation processes
in the lower layers of cratonic lithospheric mantle based on a detailed study of …

Identification of the primary compositions of mantle-derived melts is crucial for
understanding mantle compositions and physical conditions of mantle melting. However …

The processes that control water distribution in nominally anhydrous minerals from
peridotites are twofold. Melt depletion will remove water while metasomatism can potentially …

The Earth's mantle redox state regulates the fate and transfer of metals by magmatism,
buffers the igneous inputs of volcanic gases in the atmosphere and controls the depth of …

Oxygen fugacity (fO2) and temperature variations in a complete lithospheric mantle section
(70–220km) of the central Siberian craton are estimated based on 42 peridotite xenoliths in …