地震地质 ›› 2005, Vol. 27 ›› Issue (4): 609-614.

• 研究论文 • 上一篇    下一篇

K-Ar和Ar-Ar方法的精细测年及其检验

李大明, 李齐, 郑德文   

  1. 中国地震局地质研究所, 地震动力学国家重点实验室, 北京, 100029
  • 收稿日期:2005-07-27 修回日期:2005-11-07 出版日期:2005-12-08 发布日期:2009-10-26
  • 作者简介:李大明,男,1946年出生,1970年毕业于北京大学地球物理系大气物理专业,研究员,主要从事同位素地质年代学研究,电话:010-62009094,E-mail:lidaming95160326@sina.com.
  • 基金资助:
    国家自然科学基金(40273029)资助。

ACCURATE DATING AND TEST OF K-AR AND AR-AR METHODS

LI Da-ming, LI Qi, ZHENG De-wen   

  1. State Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, Beijing 100029, China
  • Received:2005-07-27 Revised:2005-11-07 Online:2005-12-08 Published:2009-10-26

摘要: 活动构造研究、近现代火山研究、古地磁研究等要求K-Ar和Ar-Ar年代学方法不断向越来越小的年龄尺度和越来越精细的方向发展。文中以腾冲等火山地区的K-Ar和Ar-Ar年代学研究结果及实验方法研究结果为根据,对K-Ar和Ar-Ar方法的精细测年及其检验进行阐述。说明K-Ar和Ar-Ar年代测定结果是单个样品的单次测量结果,其影响因素包括样品因素和实验因素。为了提高测年结果的准确度和精确度,必须有严格而合理的野外采样和实验过程,并且在具体的地质样品年代测量之外,还应经常利用一系列可能的方法对实验结果进行检验。

关键词: K-Ar, Ar-Ar, 精细测年, 检验

Abstract: The K-Ar and Ar-Ar dating methods are the developed methods and widely applied to various geosciences'fields. Study on the active tectonics,latter-day volcanoes and paleo-geomagnetism requires that the K-Ar and Ar-Ar methods should be developed towards the accurate dating and small time-scale. In recent years,geologists have paid much attention to dating the Tongchang volcano,Changbaishan volcano and Wadalianchi volcano in China and acquired many achievements. So it is practically significant to study and summarize the K-Ar and Ar-Ar methods and their test for accurate dating. The key to accurate dating is: (1) appropriate sample; (2) strict pretreatment; and (3) proper measurement. In detail,the appropriate sample is that the sample can stand for right geological meanings and it is examined to be fresh under microscope over rock slice. The pretreatment is a complex process and is very important. For example,the age of raw volcanic rock in eastern slop of Maanshan is 0.18?0.08Ma and 0.45?0.32Ma due to the effect of excess argon in crystal. However,by picking out the olivine and plagioclase crystal,the age is 0.025?0.004Ma,0.028?0.006Ma and 0.030?0.005Ma,showing a good consistency. The useful method to test the validity of the measurement process is the repeated measurement of standard sample and geologic specimen. At the same time,the difference between the repeatedly measured results should be less than the theoretic error. For example,the repeatedly measured results of the two samples from Maanshan are 0.028?0.006Ma and 0.030?0.005Ma,0.030?0.005Ma and 0.036?0.005Ma,and 0.046?0.004Ma and 0.050?0.003Ma,respectively. In addition,inter-lab comparison and inter-chronology comparison are valid methods,too. The result of K-Ar and Ar-Ar dating usually is the value which is measured one time from one sample. There are two factors,including sample and measurement,which affect the result. In order to improve the accuracy of measurement,the sampling and experiment process should be reasonable and stringent. In addition,it is necessary to test out the result by a series of methods,such as inter-chronology comparison,inter-lab comparison and geological feature.

Key words: K-Ar, Ar-Ar, accurate dating, test

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