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济阳坳陷第三系地层中自生磷灰石的裂变径迹年龄测定
引用本文:戴贤忠,王庆隆.济阳坳陷第三系地层中自生磷灰石的裂变径迹年龄测定[J].地质科学,1993,28(3):283-287.
作者姓名:戴贤忠  王庆隆
作者单位:1. 胜利油田地质科学院, 东营257015;2. 国家地震局地质研究所, 北京100029
摘    要:经电镜分析发现,胜利油田主要产油(气)的第三系沉积岩中存在少量自生磷灰石,其特征为:具有自形或半自形;颗粒周围无风化晕圈;沿大的裂隙也无风化晕带。作者采用裂变径迹法对该自生磷灰石作了单颗粒年龄测定。实践证明,裂变径迹法测定年轻沉积地层的年龄是可行的。

关 键 词:裂变径迹  热事件  退火带
收稿时间:1990-11-01
修稿时间:1990-11-01;

FISSION TRACK DATING OF AUTHIGENIC APATITE FROM TERTIARY SEDIMENTS IN THE JIYANG DEPRESSION, SHANDONG
Dai Xianzhong Du Yunhua.FISSION TRACK DATING OF AUTHIGENIC APATITE FROM TERTIARY SEDIMENTS IN THE JIYANG DEPRESSION, SHANDONG[J].Chinese Journal of Geology,1993,28(3):283-287.
Authors:Dai Xianzhong Du Yunhua
Institution:1. Academy of Geological Science of Shengli Oil Field, Shandong Dongying 257015;2. Institute of Geology, State Seismological Bureau, Beijing 100029
Abstract:Fission track age of authigenic apatite from twentytwo samples of the Jiyang Depression have been determined and the results was compared with of paleomagnetic and K-Ar age data. The agreeement between the age data indicates that the method is feasible for age determination of sediments. The paper also suggested a new division of Guantao basal conglomerate.
Keywords:Fission track  Thermal event  Annealing zone  
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