Radiochemistry
Ar-Ar dating, or Argon-Argon dating, is a radiometric dating method that determines the age of rocks and minerals by measuring the ratio of radioactive isotopes of argon. This technique is an advancement over the K-Ar dating method, allowing for more precise age determinations by comparing the amounts of 39Ar and 40Ar in a sample. It’s particularly useful for dating volcanic rocks and provides a way to establish a timeline for geological events.
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