The CHONS elements that constitute the outgassed atmosphere and exosphere have likely
been delivered by chondritic materials to the Earth during planetary accretion and …

Petit-spot volcanoes provide a unique opportunity to directly examine the structure and
geochemical composition of the lithospheric and asthenospheric mantle beneath the …

Most magmatism occurring on Earth is conventionally attributed to passive mantle upwelling
at mid-ocean ridges, to slab devolatilization at subduction zones, or to mantle plumes …

Crucial monitors of operation of deep Earth volatile cycles are the accumulated volatile
masses in the exosphere, particularly when these are compared to outgassing fluxes and to …

To determine partitioning of C between upper mantle silicate minerals and basaltic melts, we
executed 26 experiments between 0.8 and 3 GPa and 1250–1500° C which yielded 37 …

In order to better determine the behavior of CO 2 relative to incompatible elements, and
improve the accuracy of mantle CO 2 concentration and flux estimates, we determined CO 2 …

The deep carbon cycle plays an important role on the chemical differentiation and physical
properties of the Earth's mantle. Especially in the asthenosphere, seismic low-velocity and …

Petit-spot volcanism is a phenomenon ubiquitous on Earth. It originates from melt in the
upper-most mantle asthenosphere, occurring where the plate flexes and fractures before …

The origins of ferromanganese (Fe–Mn) crusts that form in seawater and elemental
partitioning into these crusts have previously been studied using samples from water depths …

Areas of old and cold oceanic plate lack conventional volcanism and have been assumed to
be devoid of submarine hydrothermal activity. However, petit-spot volcanoes are common in …