基本信息
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职业迁徙
个人简介
Geochronology is the science of determining the ages of rocks, minerals and other materials from the Earth and other Solar System bodies. The ages are determined by measuring the amounts of a radioactive isotope with a known half-life and its decay product. Geochronology allows us to determine which of the geological events close in time occurred first, and thus to constrain their causal relations. It also enables us to measure the rates of geological processes that occurred in the past.
Research Interests
Isotopic dating (geochronology) of terrestrial and extraterrestrial materials and processes.
Advancement of techniques for isotope analysis.
Formation and early evolution of our Solar System.
Early evolution of the Earth's crust and mantle.
Refining decay constants and other fundamental parameters of radiogenic isotope geochemistry.
Migration and partitioning of elements.
Disequilibrium in U and Th decay series, and its application as a geochronometer and isotopic tracer.
Radiation effects in solids.
研究兴趣
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Journal of Analytical Science and Technologyno. 1 (2024): 1-25
ICARUS (2024): 115884
Meteoritics & Planetary Science (2024)
The Planetary Science Journalno. 8 (2023): 144-144
METEORITICS & PLANETARY SCIENCE (2023): A173-A173
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SCIENCE ADVANCESno. 45 (2023)
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