The La-138 beta- decay constant was determined geophysically. The isotopic
growths of Ce-138/Ce-142 and Nd-143/Nd-144 were examined from ancient igneo
us crystalline rocks. For the Ce isotope measurement, a newly developed dyn
amic multicollector technique was applied. The crystallization age of the r
ocks was calculated to be 2037+/-13 Myr from the growth of Nd-143. From the
age and the growth of Ce-138, lambda(beta) of La-138 was estimated to be (
2.37+/-0.10) x 10(-12) yr(-1). This value is consistent with those of the l
atest two gamma-ray counting data of lanthanum compounds within the analyti
cal error.