Over long periods of time (~ Ma), we may consider the oceans, atmosphere and biosphere
as a single exospheric reservoir for CO2. The geological carbon cycle describes the inputs …

The major magmatic volatile components—H2O, CO2, S, Cl, and F—play an important role
in the formation, evolution, and eruption of magma. Knowledge of magmatic concentrations …

Alkaline mafic magmas forming intra-plate oceanic islands are believed to be strongly
enriched in CO2 due to low-degree partial melting of enriched mantle sources. However …

Skeletal muscle exhibits great plasticity in response to altered activity levels, ultimately
resulting in tissue remodelling and substantial changes in mass. Animal research would …

Volcanoes emit larger amounts of volcanic gas than can be dissolved in the volume of
erupted magma during a variety of volcanic processes, including explosive and effusive …

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 …

The ordinarily benign activity of basaltic volcanoes is periodically interrupted by violent
paroxysmal explosions ranging in size from Hawaiian to Plinian in the most extreme …

This review aims at summarizing currently available data on fluid inclusions and melt
inclusions from Climax-type porphyry Mo deposits. Data are presented from 16 economically …

Volcanic degassing represents an essential component of the global geochemical cycles
that determine the state of the atmosphere and climate. It also exerts a first-order influence …