Fluids in the deep crust and upper mantle appear to have played roles in the long-term
evolution of the subcratonic lithospheric mantle and the stabilities of the continents, in the …

The partitioning of major and trace elements between eclogite and aqueous fluids with
variable salinity was studied at 700–800° C and 4–6 GPa in piston cylinder and multi anvil …

Previous studies have concluded that dehydration of serpentinites in subduction zones
produces oxidizing fluids that are the cause of oxidized arc magmas. Here, observations of …

The number of solute species required to describe the thermodynamic behavior of
electrolytic fluids is a hindrance to the incorporation of aqueous geochemistry in petrological …

Bingham Canyon is one of the world's largest porphyry Cu–Mo–Au deposits and was
previously used as an example to emphasize the role of magma mixing and magmatic …

This paper explores bulk-rock geochemical data for a wide array of metamorphosed mafic,
quartzo-feldspathic, pelitic, and metacarbonate rocks using a quantitative mass-balance …

Processes taking place in subduction zones are the main controller of the chemical cycle of
volatile and incompatible elements in the Earth system. Metamorphic devolatilization …

Carbon is subducted to depths where metamorphism liberates water-bearing fluids. The C-
bearing fluids facilitate partial melting of the upper mantle, generating magmas that may …

Abstract Negative Cerium (Ce) anomalies are observed in chondrite-normalized Rare Earth
Element patterns from various volcanic arc suites. These anomalies are well defined in …

Cretaceous continental eclogites of the Chuacús Complex (Guatemala Suture Zone) contain
an extensive record spanning more than 1.1 Ga. In this study, we combine U-Pb zircon …