绿泥石的裂变径迹退火及年龄测定

O.P. Sharma, K.D. Bal, K.K. Nagpaul
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引用次数: 14

摘要

为了得到可能经过地质退火的绿泥石年龄的校正因子,进行了系统的退火实验。矿石中所有的轨迹都在500度下加热一小时退火。实验数据的外推表明,160°c的温度需要106年才能去除绿泥石中的所有痕迹。6个样品的年龄已经确定。印度安得拉邦Nellore的校正年龄为606±17 × 106 y,与裂变径迹法测定的共存矿物年龄吻合较好。绿泥石的活化能范围为1.2 ~ 2.0eV,平均值为1.5 eV。
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Fission track annealing and age determination of chlorite

Systematic annealing experiments have been carried out in order to obtain correction factors for the ages of chlorite, which may have undergone geological annealing. All the tracks in the mineral are annealed by heating for one hour at 500°. Extrapolation of experimental data suggests that a temperature of 160° would be required for 106 years to remove all the tracks in chlorite. Ages of 6 samples have been determined. The corrected age of 606 ± 17 × 106 y obtained for Nellore, Andhra Pradesh, India, agrees well with the ages of coexisting minerals, determined by the fission-track method. The activation energy for chlorite ranges from 1.2 to 2.0eV, with a mean value of 1.5 eV.

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