The Building of New Isotope Fractionation Theories in High-Temperature Processes

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Key Points

The aim is to develop new theories on isotope effects in high-temperature geological processes to address key scientific challenges.
Developed new theoretical models on isotope effects, including balance and kinetic fractionation theories.
Focused on three high-temperature processes: volatilization, fractionation under thermal gradients, and magma differentiation.
Provided new fractionation formulas and analysis of isotope anomalies in geological settings.
Introduced new theories for isotopic behaviors in high-temperature conditions that have been peer-validated.
Presented applications for estimating reservoir sizes and remelting processes using isotopic signals.
Established a framework for understanding the implications of these new models on geological research.

Theoretical advancements in isotope effects enhance understanding of geological and planetary sciences.

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LIU et al. (2026) studied this question.

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