Many studies exist on magmatic volatiles (H, C, N, F, S, Cl) in and on the Moon, within the
last several years, that have cast into question the post-Apollo view of lunar formation, the …

The end-Triassic mass extinction (ETME) is thought to have been caused by voluminous,
pulsed volcanic activity of the Central Atlantic Magmatic Province (CAMP). Over the last …

This study, via combined analysis of geophysical and geochemical data, reveals a
lithospheric architecture characterized by crust–mantle decoupling and vertical heat-flow …

Despite its relatively minor abundance in magmas (compared with H2O and CO2), sulfur
degassing from volcanoes is of tremendous significance. It can exert substantial influence …

Stromboli is known for its persistent degassing and rhythmic strombolian activity
occasionally punctuated by paroxysmal eruptions. The basaltic pumice and scoria emitted …

Processes controlling the composition of seafloor hydrothermal fluids in silicic back-arc or
near-arc crustal settings remain poorly constrained despite growing evidence for extensive …

Recent discoveries of water-rich lunar apatite are more consistent with the hydrous magmas
of Earth than the otherwise volatile-depleted rocks of the Moon. Paradoxically, this requires …

The transition to a low-carbon economy will increase demand for a wide range of metals,
notably copper, which is used extensively in power generation and in electric vehicles …

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

We conducted a petrologic study of apatite within 12 Martian meteorites, including 11
shergottites and one basaltic regolith breccia. These data were combined with previously …