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Updated: Sep 11, 2025

Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
Leveraging radioisotope geochronology and diffusion chronometry to trace the thermal evolution of magmatic systems
Wei-Ran Li1,2, Fidel Costa3
1VRock Laboratory, Department of Earth Sciences, The University of Hong Kong, China.
Abstract:
Time scales determined by radioisotope geochronology and diffusion chronometry for the same magmatic systems have shown variable degrees of discrepancy. We show in this paper that this could be due to the different temperature ranges that the two types of chronometers are effectively sampling, therefore combining them will help to trace the thermal evolution of magmatic systems on Earth and other planets.
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