Geochemistry
Ar-Ar dating, or argon-argon dating, is a radiometric dating technique used to determine the age of rocks and minerals by measuring the ratio of radioactive isotopes of argon. This method relies on the decay of potassium-40 to argon-40, which allows scientists to date geological events with high precision. It is particularly useful in dating volcanic rocks and has enhanced our understanding of geological time scales and the history of Earth's formations.
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