40Ar-39Ar同位素定年方法研究进展  

Advances in the study of 40Ar-39Ar isotopic dating method

作　　者：张佳[1] 刘汉彬[1] 李军杰[1] 金贵善[1] 韩娟[1] 张建锋[1] 

机构地区：[1]核工业北京地质研究院,北京100029

出　　处：《世界核地质科学》2014年第1期53-58,共6页World Nuclear Geoscience

基　　金：中国核工业集团公司地矿事业部铀矿地质科研项目"华东南热液型铀矿成矿时代与成矿温度研究"资助(编号:测D1101)

摘　　要：40Ar-39Ar同位素定年法是由K-Ar法发展而来,通过将39K利用快中子辐照衰变成39Ar,测量40Ar*/39Ar来获得年龄值。经过长期发展,该方法的测试技术逐渐成熟,其中气体提取发展为常规阶段升温法、激光显微探针法以及真空压碎流体包裹体法;气体纯化主要有冷阱去除法、钛泵吸附法、锆铝泵吸附法;气体测试的质谱仪也在灵敏度、分辨率、背景值等技术指标上有很大提高。40Ar-39Ar同位素定年法在石油、固体矿产等方面应用广泛,尤其在油气成藏时间、成岩成矿作用时间的热年代学研究等领域。^40Ar-^39Ar isotopic dating method is developed from K-Ar method which irradiate ^39K into ^39Ar by fast neutron and measure ^40Ar^＊/^39Ar to get the age value. After a long-term development, testing technologies of this method is matured, gas extraction stage has been developed into the conventional step-heating method, laser microprobe law as well as fluid inclusions vacuum crushing method. Gas purification methods mainly contain cold trap removal method, titanium pump adsorption method and zirconium-aluminum pump adsorption method. For gas testing, some technical indicators of mass spectrometers have greatly improved, especially in sensitivity, resolution, background. ^40Ar-^39Ar isotopic dating method is widely applied in the fields of petroleum, solid minerals, etc., especially in thermochronology for hydrocarbon accumulation time, diagenetic time, mineralization time.

关 键 词：^40Ar-^39Ar法 同位素定年 地质应用 研究进展 

分 类 号：P597.1[天文地球—地球化学] O657.63[天文地球—地质学]