Zhaxikang is one large Sb–Pb–Zn–Ag deposit located in the North Himalaya of southern
Tibet. To date, the genesis of this deposit still remains controversial. Here, we present new …

Central to understanding the processes that drive stable isotope fractionation in nature is
their quantification under controlled experimental conditions. The polyvalent element iron …

Skarn deposits are major repositories of Fe and are the principal sources for iron mining in
China. However, their mechanism of formation remains debated. Here we investigate the …

The origin of heavy Fe isotope compositions in high-silica (> 70 wt% SiO 2) igneous rocks
remains a highly controversial topic. Considering that fluid exsolution in eruptive rocks is …

Abstract Continental intraplate basalts (15.42–0.16 Ma) from Abaga–Dalinuoer volcanic field
(ADVF) in central Inner Mongolia of eastern China, as a part of Cenozoic volcanic province …

Abstract Separation of Fe–Ti oxides during magmatic differentiation plays an important role
in controlling Fe isotopic evolution of residual magmas. Titanomagnetite (Tmag) is a …

To investigate the petrogenesis of Fe-Ti oxide ore deposits, we report Mg and Fe isotopic
compositions for coexisting olivine, clinopyroxene and ilmenite in Fe-Ti oxide ores …

Iron isotopes of magnetite have been used to unravel the sources and evolutionary
processes of magma and ore deposits, but most studies have focused on bulk-rock samples …

In order to investigate how Fe was enriched from parental high‐Ti basaltic magma to form
the stratigraphically thick Fe‐Ti oxide ore at the bottom layers, we present a systematic study …

Abstract The Xiarihamu Ni-Co sulfide deposit in the East Kunlun orogenic belt (EKOB),
western China, is the largest magmatic Ni-Cu-(Co) sulfide deposit found in the orogenic …