As a component of many minerals and an essential trace element in most aerobic
organisms, the transition metal element Cu is important for studying reduction-oxidation …

The Hattu schist belt is located in the western part of the Archaean Karelian domain of the
Fennoscandian Shield. The orogenic gold deposits with Au–Bi–Te geochemical signatures …

In order to characterize antimony (Sb) isotope fractionation in hydrothermal systems, we
present Sb isotope compositions of primary stibnite ores from a large Sb deposit in south …

The use of copper isotopes related to ore deposit location and genesis has greatly
expanded over the past twenty years. The isotope values in ores, rocks, soils, and water …

Abstract The Tuwu porphyry Cu deposit is located in the northern segment of the Jueluotage
metallogenic belt in Eastern Tianshan, on the southern margin of the Central Asian orogenic …

Although it has been recently demonstrated that Cu isotope fractionation during mantle
melting and basaltic magma differentiation is limited, the behavior of Cu isotopes during …

The characterisation of relative copper isotope amount ratios (δ65Cu) helps constrain a
variety of geochemical processes occurring in the geosphere, biosphere and hydrosphere …

We analyzed the first Cu isotopes in primary cupreous pyrite and orpiment, from modern
CO2-degassing, seafloor massive sulfide diffuser vents (“KCO2Ds”), from the Kolumbo …

Abstract High-silica granites (> 74 wt% SiO 2) in the Nanling Range are associated with
important W–Sn deposits. Their petrogenesis remains controversial. The Qitianling …

A compilation of copper isotopic compositions (δ65Cu) from supergene systems suggests
distinct differences in the mean δ65Cu of Cu in leach cap (δ65Cu=− 1.2±3.5‰), enrichment …