• 责任者：Zhang Xiangtao (China Limited Shenzhen ; CNOOC ; Shenzhen 518067 ; China) ; Zhang Qinglin
• 刊名：Geology and Mineral Resources of South China
• 出版年：2012
• 卷期：28(2)
• 关键词：裂变径迹计时 ; fission-track dating
• 页码：p.93-99
• 图表：3 illus., 35 refs.
• 分类号：0900
• issnNo：ISSN1007-3701
• isbnNo：CN42-1417/P

Fission-track (FT) thermochronology is a low-temperature dating technique utilizing the damage property produced by uranium fission decay. As the advanced researches of annealing behavior, and laboratory annealing models, this technique, especially apatite fission-track, has become an important measure to constrain the thermal history of sedimentary basin. Among three main apatite fission-track annealing models proposed by Laslett et al.（1987）, Crowley et al.（1991） and Ketcham et al.（1999）, respectively, the last one is the most significant and widely-applied annealing model, which integrated the influence of time, temperature and chemical composition to various types of apatite, together using the c-axis projected track-length and D_par.