摘要
裂变径迹法是上个世纪60年代兴起的低温热年代学方法。裂变径迹法早期以定年为主,随着裂变技术的发展,这种方法广泛应用于造山带的研究,包括:造山带隆升时代和隆升速率的研究、造山带热演化历史模拟研究。
Fission track method as a geological dating tool was firstly proposed in the early 1960s. In the past decades there has been a major expansion in application of fission track dating. As the development of fission track technique, it has been applied to the study of oregenic belt widely, including: to determine the uplifting time and rate of orogenic belt and to study the thermal history of orogenic belt.
出处
《自然科学》
2017年第2期246-252,共7页
Open Journal of Nature Science
