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1. 中国科学院高能物理研究所
2. 核工业北京地质研究院
3. 中国原子能科学研究院
4. 中国科学院广州地球化学研究所
5. 中国科学院高能物理研究所核工业北京地质研究院中国原子能科学研究院中国科学院广州地球化学研究所
Published:01 October 1996
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[1]翟鹏济,赵云龙,郝秀红,胡瑞英.裂变径迹定年实验室标准化刻度[J].核技术,1996(10):629-631.
Zhai Pengji. Laboratory standardization for fission track dating calibration[J]. Nuclear techniques, 1996, (10).
用第六届国际裂变径速测定地质年代学术讨论会推荐的锆石、磷灰石和榍石年龄标样和SRM612铀玻璃刻度了Zeta值。三种矿物的Zeta值差异不大,与加权平均339.2±6.6(2σ)接近。将Co箔法测得的Φ值与用自行刻度的b值测标准铀玻璃在白云母上诱发径迹密度计算得到的Φ值进行了比较.利用外探测器方法测定了裂变径迹定年国际标样中三种锆石和两种磷灰石的年龄,其结果与推荐的参考年龄在误差范围内一致.
In this paper several age standards (including three zircon
two apatite and one sphene) have been used for Zeta determination against SRM612. No significant difference of three minerals is found. A single-weighted mean Zeta constant is given as 339.2±6.6(2σ).The thermal neutron flux calculated from σ Φ is compared with that determined from Co foil. The ages of zircon and apatite are determined using the calibrated constant b and the track density by a dosimeter glass. The results of 27.7±0.8Ma for FCT
16.1±0.5Ma for MB
60.0±3.0Ma for TR and 30.8± 1.9Ma for Durango are consistent with the reference ages within the range of error.
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