Proportional retention of I and radiogenic Xe-129 in preheated Allende

In order to study the effects of heat loss and redistribution of iodine and xenon on the I-Xe age, the iodine-xenon dating technique was applied to a bulk sample of the Allende chondrite and a similar sample preheated to 900 C prior to the irradiation. Little iodine or Xe-129 were lost from the high-temperature fractions of the preheated sample, and the high-temperature isochron was fully preserved. The amounts of I and radiogenic Xe-129 retained by the preheated sample were nearly proportional in those temperature fractions (900-1150 C) where most I and radiogenic X-129 were lost. However, the intermediate-temperature isochron was modified, resulting in an apparent isochron which would predate the high-temperature isochron by 6.7 + or - 1.1 m.y.