Sphalerite has been recognized as the most important carrier mineral of the critical metal of
indium (In), which mainly exists in sphalerite lattice through isomorphous substitution for Zn …

Stable Ce isotope ratios are considered potential indicators for tracing the redox state of
Earth's surface; however, their quantitative relationship remains undefined. Here, we …

Rare earth elements (REEs) have been found to have numerous uses to trace geological
and cosmochemical processes through analyses of elemental patterns, radioactive decay …

Eu isotopes are promising tracers across various scientific domains such as planetary, earth,
and marine science, yet their high-precision analysis has been challenging due to the …

The nuclear volume component of equilibrium field shift isotope fractionations in europium
and other lanthanide elements is estimated using Mössbauer spectroscopy and electronic …

Stable Nd isotope ratios are regarded as a potential tracer for marine rare earth elements
(REEs) cycling. However, the fractionation behavior of Nd in marine geological processes …

Quantifying equilibrium Sn isotope fractionation among Sn-bearing minerals is fundamental
for understanding the partitioning of Sn isotopes during various geological and …

Eu isotopes are recognized as potential indicators for understanding continental crust
evolution, ocean circulation, and rare earth element mineralization. However, methods for …

Eu isotope ratio can be precisely measured by MC-ICP-MS using a Sm isotope pair as spike
for normalization. The standard chemical reagent NIST3117a exhibits almost no Eu isotope …

Equilibrium cerium isotope fractionations in cerium-bearing minerals and aqueous species
are estimated using electronic structure calculations that include both nuclear volume and …