Geochemistry articles for University of Science and Technology of China (USTC), China

Time frame: 1 June 2025 - 30 May 2026

View topic

Count: 18

Article ‘Count’ for Geochemistry.

Journal Count Share
2 0.11
A Novel Strategy for Synthesizing Matrix-Matched Microanalysis Reference Materials via Hydrothermal Precursors and Ultrahigh-Pressure Sintering 0.05
A Low-Background, High-Flatness Mounting Method for In Situ SIMS Isotopic Analysis for Fine-Grained Samples 0.06
1 0.64
Underestimated legacy of historical metallurgy and modern contamination transformation in southwestern China: insights from crater lake sediments 0.64
12 3.60
The impact of forearc serpentinization on the composition of subduction-zone fluids revealed by Mg–Fe isotopes in jadeitites 0.28
Contrasting Cu isotope signatures in arc magmas and lower continental crust: insights into deep crust copper reservoir 0.36
Kinetic isotope fractionation during crystal growth 0.43
Fluid-mediated Zr transfer in subduction zones: constraints from extreme Zr isotope fractionation in an ultrahigh-pressure eclogite–vein system in the Dabie orogen 0.50
Significant Mg isotope disequilibrium during crustal anatexis: Implications for heterogeneous Mg isotopic compositions in the continental crust 0.56
Zircon records carbonatite fractional crystallization and hydrothermal metasomatism during REE mineralization 0.15
Silicon isotope variations of ocean island basalts: the effect of recycled materials on Si isotopes in the mantle 0.22
Zircon solubility modulated by boron in hydrous granitic melts 0.50
Chalcophile elements in post-subduction magmas and implications for metal recycling in oceanic and continental subduction 0.11
Potassium isotopic equilibrium fractionation induced by clay adsorption and incorporation: A density functional theory study 0.01
Barium isotope variation during granitic magma differentiation: implications for the discrimination of crystal fractionation and fluid-magma interaction 0.42
Links between forearc decarbonation and generation of high δ26Mg fluids at subarc depths: constraints from carbonate-bearing forearc serpentinites 0.07
1 0.50
Fe isotope decoding of fluid-absent versus fluid-present melting of deeply subducted continental crust 0.50
1 0.30
Tracing Mantle Sources to Tectono–Magmatic Settings: Machine Learning Classification of Basalts Over the Past 1 Billion Years 0.30
1 0.13
Plume-induced emissions of deep methane linked to the end-Guadalupian mass extinction 0.13

Numerical information only (in the tables above) is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International.