ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
北京石花洞地区奥陶纪灰岩36Cl侵蚀速率初探
  
关键词:surface erosion rate of limestone 36Cl AMS
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作者单位E-mail
晁念英 中国地质大学环境学院湖北 武汉430072 nychao@cug.net.cn 
潘欢迎 中国地质大学环境学院湖北 武汉430072  
刘存富 中国地质大学环境学院湖北 武汉430072  
万军伟 中国地质大学环境学院湖北 武汉430072  
王佩仪 中国地质大学环境学院湖北 武汉430072  
姜山 中国原子能科学研究院核物理研究所北京102413  
何明 中国原子能科学研究院核物理研究所北京102413  
武绍勇 中国原子能科学研究院核物理研究所北京102413  
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摘要:
A Preliminary Study of 36Cl Erosion Rates of Ordovician (O2)Limestone in Shihuadong Area. Beijing
      In this paper five sources of 36Cl in limestone are theoretically studied, and four characteristics of 36Cl distribution in deep limestone profile are discussed. The sampling method of 36Cl and the AMS analytical technique are described in detail. The surface erosion rate of limestone is Shihuadong area of Beijing is calculated(ε=17.40μm/a).
SHAO Nianying,PAN Huanying,LIU Cunfu,WAN Junwei,WANG Peiyi,JIANG Shan,HE Ming,WU Shaoyong.2005.A Preliminary Study of 36Cl Erosion Rates of Ordovician (O2)Limestone in Shihuadong Area. Beijing[J].Acta Geoscientica Sinica,26(z1):272-274.
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