摘要
文章描述了磷灰石(U-Th)/He热年代学方法的基本测年原理、校正模型、封闭温度和实践验证,及此方法在古地形演化、山体剥露历史和剥蚀速率研究中的应用。
The basic principle of apatite (U-Th)/He thermochronomety, dating method, model for correcting He age, closure temperature and the empirical studies, were described in this paper. Its applications in studies of paleo-geomorphology, exhumation history of orogens, and erosion rate were also described.
出处
《原子能科学技术》
EI
CAS
CSCD
北大核心
2008年第7期662-664,共3页
Atomic Energy Science and Technology
基金
国家重点基础研究发展规划项目(2005CB422001)
国家自然科学基金优秀创新群体项目(40421101)