摘要
测定了我国11个H型、6个L型和3个LL型球粒陨石的热释光特征。H型球粒陨石的TL峰温和峰宽分别为163-206℃平均和83-137℃平均,L型和LL型球粒陨石分别为183-203℃平均和111-143℃平均。依据TL数据和已发表的稀有气体同位素数据,引入了(3He暴露年龄/21Ne暴露年龄)-诱发TL灵敏度-(4He气体保存年龄/40Ar气体保存年龄)图,这种图形是鉴别不同陨石热历史的一种有效方法。
Induced thermoluminescence(TL)properties of Chinese 11H,6L and 3LL chondrites have been measured.TL peak temperature and peak width are 163-206℃,Av.and 83-137℃ for H chondrites,183-203℃,and 111-143℃,for L and LL,respectively. Recently fallen Chinese ordinary chondrites have TL peak width generally smaller than those of ordrinary chondrites from other regions.Based on our TL sensitivity data and published noble gases data, a 3He exposure age/21Ne exposure age-Induced TL sensitivity-4He gas retention/40Ar gas retention diagram is introduced. This type of diagram is a powerful tool for distinguishing different thermal histories of meteorites.
出处
《核技术》
CAS
CSCD
北大核心
1995年第7期399-404,共6页
Nuclear Techniques
基金
国家自然科学基金
关键词
陨石
热历史
热释光
稀有气体
中国
Ordinary chondrites, Induced thermoluminescence,Thermal history