论文部分内容阅读
测定地质年龄的裂变径迹方法是60年代才开始发展起来的一种新方法。由于该方法测定的年龄范围很宽:样品适应性广:分析中消耗的样品量少;不需要质谱计分析,因此在许多领城(如地质年代学、宇宙年代学、地球物理、海洋地质、第四纪地质、构造地质、考古等)得到了愈来愈广泛的应用。《裂变径迹年龄测定》一书是由中国科学院地球化学研究所刘顺生、张峰、胡瑞英、刘京发编著、地
The fission track method for determining geologic ages was a new method that began to develop in the 1960s. Due to the wide range of ages determined by this method, the wide range of samples is adaptable: the small sample amount consumed in the analysis and the absence of mass spectrometry analysis. Therefore, in many terrains (eg geochronology, cosmochronology, geophysics, marine geology, Quaternary geology, tectonic geology, archeology, etc.) have been more and more widely used. “Fission track age determination,” a book by the Institute of Geochemistry, Chinese Academy of Sciences Liu Shun, Zhang Feng, Hu Ruiying, edited by Liu Jingfa,