This work focuses on a rigorous analysis of the physical–chemical, compositional and
textural relationships of amphibole stability and the development of new thermobarometric …

Subduction zones are where sediments, oceanic crust, and mantle lithosphere return to and
reequilibrate with Earth's mantle. Subduction zones are interior expressions of Earth's …

Interactions between crustal and mantle reservoirs dominate the surface inventory of volatile
elements over geological time, moderating atmospheric composition and maintaining a life …

Carbon geochemistry of mantle-derived samples suggests that the fluxes and reservoir sizes
associated with deep cycle are in the order of 1012–13gC/yr and 1022–23g C, respectively …

Spring temperatures in temperate regions have increased over the past 20 years, and many
organisms have responded to this increase by advancing the date of their growth and …

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 …

Subduction zones generate voluminous magma and mediate global element cycling. Fluids
are essential to this activity, yet their behavior is perhaps the most poorly understood aspect …

Subducted crust refertilizes the subarc mantle wedge as well as the deep convecting mantle.
In the subarc region, mass transfer occurs mainly through fluids, melts, or supercritical …

The term" carbon cycle" is normally thought to mean those processes that govern the
present-day transfer of carbon between life, the atmosphere, and the oceans. This book …

Subduction zones modulate the global carbon cycle. Carbon is transported into the mantle
by the subducting slab and returned to the surface by degassing at arc volcanoes above the …