A method for dating clays is important for studies of weathering, diag
enesis, hydrocarbon migration, and the formation of major metalliferou
s deposits. However, many attempts have produced imprecise or inaccura
te results. Data from shales show that, contrary to expectations, the
Ar-40-Ar-39 dating technique can be successfully used to determine the
diagenetic age of ancient sediments because Ar-39 losses during irrad
iation are controlled by release from low retentivity sites in illite
equivalent to those that have lost radiogenic Ar-40 in nature, rather
than by direct recoil as is generally assumed.