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 …

The Maoniuping giant rare earth element deposit is genetically related to a Cenozoic
alkaline syenite–carbonatite complex. However, the origin of the alkaline complex and the …

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

Molybdenum isotope variations in mafic arc lavas have mainly been attributed to the
influence of slab-derived components, such as subducted sediment melts and aqueous …

Molybdenum isotopes have emerged as novel tracers for high-temperature igneous and
metamorphic processes. The debate remains to what extent different subducted slab …

Mid-ocean ridge basalts (MORB) reveal large mantle compositional heterogeneity, whose
origin remains debated. Here we present a systematic study of molybdenum isotopes on …

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 …

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 …