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

作　　者：付潮罡 

机构地区：[1]广州市地质调查院,广东广州

出　　处：《自然科学》2017年第2期246-252,共7页Open Journal of Nature Science

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.

关 键 词：裂变径迹法 造山带 隆升 热历史 

分 类 号：P61[天文地球—矿床学]