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.
付潮罡. 裂变径迹法测年概述及其在造山带研究中的应用Fission Track Dating Method and Its Application to the Study of Orogenic Belt[J]. 自然科学, 2017, 05(02): 246-252. http://dx.doi.org/10.12677/OJNS.2017.52033
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