地质与资源2012，Vol.21Issue(3)：308-312,5.
裂变径迹热年代学方法、应用及其研究展望
FISSION-TRACK THERMOCHRONOLOGY: Method, Application and Latest Progress
乔建新 1赵红格 1王海然1
作者信息
- 1. 西北大学大陆动力学国家重点实验室/地质学系,陕西西安710069
- 折叠
摘要
Abstract
Fission-track, which is based on the effect of uranium fission-radiation, is a kind of isotopic thermochronology method. On the basis of analyzing the theories and methods of the fission-track, the commonly used age value as well as the effect of fission-track annealing, this paper summarizes the relevant theories of the method and their application to the orogenic belt uplifting-cooling, the sedimentary basin analysis, the relationship of mountain-basin coupling, the time-limit of fault activities, the hydrothermal mineralization and so on. With reference to current studies of the fission-track thermochronology both at home and abroad, this paper also provides implication for future studies.关键词
裂变径迹/年龄值/热年代学/造山带/沉积盆地Key words
fission-track/ age value/ thermochronology/ orogenic belt/ sedimentary basin分类
天文与地球科学引用本文复制引用
乔建新,赵红格,王海然..裂变径迹热年代学方法、应用及其研究展望[J].地质与资源,2012,21(3):308-312,5.
