Zirconium, as a high field strength element, has been widely used to trace the differentiation
of terrestrial planets. It is also a major constituent in zircon, an important accessory mineral …

Zirconium (Zr) stable isotope variations occur among co-existing Zr-rich accessory phases
as well as at the bulk-rock scale, but the petrologic mechanism (s) responsible for Zr isotope …

Stable zirconium (Zr) isotope of magmatic zircons is a promising new tracer to understand
magma differentiation in the continental crust. However, magmatic processes controlling …

Zirconium is one of high field strength elements but its isotope behavior during geochemical
processes is still uncertain because of the limited database. While Zr isotopes in magmatic …

Zirconium (Zr) isotope has significant potential for tracing magmatic processes, particularly
late-stage fractionation involving fluids. However, the fractionation of Zr isotopes between …

The origin of crystal‐scale Zr isotopic variation remains enigmatic. Here, we report high‐
precision Zr isotopic compositions of thin‐sectioned and hand‐picked zircon crystals from …

We undertook Zr isotope measurements on zircon, titanite, biotite, amphibole, and whole
rocks from the La Posta pluton (Peninsular Ranges, southern California) together with trace …

Post-collisional mafic magmas are melts of mixed sources formed by the interaction between
crust and mantle. We report the first identification of metasomatic sources formed at> 200 km …

Stable zirconium (Zr) isotopes have become the focus of attention as potential tracers of
magma crystallization and differentiation processes. However, the effects of partial melting …

Abstract The Permian-Triassic mass extinction (PTME), the most severe biocrisis of the
Phanerozoic, has been widely attributed to intense volcanism. Although the Siberian Traps …