摘要
裂变径迹分析中的“ζ”年龄校正方法、外探测器方法与单颗粒年龄以及磷灰石退火的各种动力学模式的精确建立 ,使得裂变径迹分析在沉积盆地研究中得到了广泛的应用。本文在介绍裂变径迹分析的主要进展的基础上 ,着重对这一方法在沉积盆地物源研究、时间 温度历史重建。
The ' ζ ' age correction method,the external detector method and single grained ages as well as the accurate establishment of various dynamic models for apatite fission track annealing made it possible for the fission track analysis to get widespread application in the study of sedimentary basins.Based on the introduction of major progresses in fission track analysis,the application of this method in the material source study of sedimentary basins,the reconstruction of time temperature history and the estimation of denuded stratum amount was discussed.
出处
《石油实验地质》
CAS
CSCD
2001年第3期332-337,共6页
Petroleum Geology & Experiment
基金
国家自然科学基金 ( 498760 13)
教育部资助优秀年轻教师基金
高等学校骨干教师资助计划联合资助项目
关键词
物源
热史
剥蚀量
沉积盆地
裂变径迹分析
石油地质
material sources
thermal history
the amount of denudation
sedimentary basins
fission track
