Serpentinites in subduction zones are important fluid reservoirs for crust-mantle interaction
and arc magma formation. The serpentinite-derived fluids can carry fluid-mobile elements …

Abstract The Southern Atlantic-Southwest Indian ridges (SASWIR) host mid-ocean ridge
basalts with a residual subduction-related geochemical fingerprint (ie, a ghost-arc signature) …

Altered oceanic crust (AOC) plays a critical role in geochemical recycling in subduction
zones. However, identifying contributions of subducted AOC to arc magmas remains a …

Barium isotopes have been increasingly applied to trace igneous processes, but the
applications are hindered by the lack of equilibrium Ba isotope fractionation factors between …

Rubidium is a moderately volatile element with high incompatibility and fluid mobility. Its
stable isotopes have great potential in tracing various geological processes. For example …

Stable strontium and barium isotopes are potential tracers for understanding planetary
differentiation and the nature of the building blocks of terrestrial planets. Strontium and …

As a highly fluid mobile element, barium (Ba) and its isotopes are excellent tracers for fluid
associated processes in subduction zones. However, the behavior of Ba isotopes during …

Abstract Beneath Eastern Asia, the world's spatially most extensive, and possibly extremely
long-lived big mantle wedge (BMW) occurs, formed by the Izanagi-Pacific slab residing in …

This study reports barium (Ba) isotope compositions of intact altered oceanic crust (AOC)
recovered from Integrated Ocean Drilling Program (IODP) Site 1256, East Pacific Rise …

Mantle-derived, low-degree melts, such as kimberlites, carbonate-rich olivine lamproites
(CROLS), and cratonic olivine lamproites, are the main carriers of diamonds. They are rare …