The molybdenum (Mo) isotope system is a powerful tool for tracing recycled crustal
components in volcanic rocks. Existing Mo isotope data show that intraplate basalts have …

Arc volcanic rocks erupted above oceanic subduction zones generally have heavy
molybdenum (Mo) isotopic compositions, which are attributed to contributions from oceanic …

Mo isotope compositions have been increasingly used as a source tracer in magmatic
systems. Here, we investigate the relative role of subducting oceanic crust, fluid-rich sources …

The recycling of mafic oceanic crust in subduction zones represents an important geological
process to explain the geochemical diversity of the Earth's mantle. Based on radiogenic …

The control of redox conditions on the geochemical recycling process in subduction zones is
still poorly understood due to large uncertainties in oxygen fugacity (fO 2) for subducted …

The super-chondritic Mo isotopic composition of the continental crust has been attributed to
contributions from subducted oceanic slabs and/or sediments, which introduce isotopically …

Highly variable molybdenum (Mo) isotope compositions are common in mafic arc magmas
above oceanic subduction zones, but Mo isotopes of mafic magmas related to continental …

Mafic arc igneous rocks with oceanic crust-derived fluids in their mantle sources generally
show heavy Mo isotope compositions. However, these rocks may exhibit variable Mo …

Subduction redistributes elements between Earth's principal geochemical reservoirs,
modifying the chemical composition of Earth's mantle, crust, atmosphere, and hydrosphere …

Highly variable molybdenum (Mo) isotope compositions have been reported for mafic arc
volcanics above oceanic subduction zones. The heavy Mo isotope signatures of mafic arc …