Track Fading and Its Applications in Archaeology, Tectonics and Geothermal Chronology in China
Huang, Weiwen
刊名J EARTH SCI-CHINA
2013
卷号24期号:4页码:645—651
关键词FISSION FRAGMENT TRACKS PARTICLE TRACKS HISTORY APATITE
ISSN号1674-487X
通讯作者guosl@ciae.ac.cn
英文摘要Track fading is a basic phenomenon in track science and has been the source of information in geosciences. This article summarizes the knowledge of track fading and gives some examples of successful applications of track fading in archaeology, tectonics and geothermal chronology in China. The applications of track fading are classified into 5 modes: (1) mode of complete fading (annealing); (2) mode of partial fading; (3) use of the dependence of track fading on time and temperature; (4) use of the differences of track fading between coexisting minerals; and (5) use of fading-reduced track length. Track fading mechanisms hints that scientists in geothermal chronology should adopt microprobes for quantitative elemental analysis to determine the detailed chemical compositions of each mineral grain or at least of the grains from each position of geological structures in order that one becomes well aware of the relation between the track fading behavior and chemical compositions of the mineral used.
原文出处10.1007/s12583-013-0356-8
公开日期2013-11-27
内容类型期刊论文
源URL[http://119.78.100.205/handle/311034/4128]  
专题古脊椎动物与古人类研究所_古人类及旧石器研究室
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Huang, Weiwen. Track Fading and Its Applications in Archaeology, Tectonics and Geothermal Chronology in China[J]. J EARTH SCI-CHINA,2013,24(4):645—651.
APA Huang, Weiwen.(2013).Track Fading and Its Applications in Archaeology, Tectonics and Geothermal Chronology in China.J EARTH SCI-CHINA,24(4),645—651.
MLA Huang, Weiwen."Track Fading and Its Applications in Archaeology, Tectonics and Geothermal Chronology in China".J EARTH SCI-CHINA 24.4(2013):645—651.
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