摘要
利用海绿石40Ar-39Ar年龄校正公式,通过测量海绿石中的可膨胀层含量n以及中子活化过程中39Ar的丢失率,求出海绿石的年龄。经测定,京津地区铁岭组、景儿峪组海绿石中可膨胀层含量为5%~6%,中子活化中39Ar丢失率为17%~19%。由校正后的海绿石年龄推测出铁岭组年龄界限范围是1070±10Ma~1175±10Ma,景儿峪组为810±10Ma~900±10Ma。
The glauconites from Tieling Fm.and Jingeryu Fm. Beijing-Tianjin Area,contain 5%~6% expandable layer, and the lost rate of 39Ar during neutron irradiation is between 17% and 19%.From these data and the corrected formula for,40Ar-39Ar dating of glauconites deduced by the authors in other paper,the ages of the glauconites from these two Formations are calculated. The corrected ages of the glauconites from Tieling Fm. are between 10821±13Ma and 1171±11Ma and those from Jingeryu Fm. are between 816.1±8.9Ma and 880.0±8.5Ma,from which the authors suggest that the age range of Tieling Fm. is 1070±10Ma to 1175±10Ma and that of Jingeryu Fm. is 810±10Ma to 900±10Ma.
出处
《岩石学报》
SCIE
CAS
CSCD
北大核心
1996年第3期416-423,共8页
Acta Petrologica Sinica
基金
国家自然科学基金
关键词
海绿石
氩同位素
年龄
铁岭组
景儿峪组
Glauconite
 ̄40Ar- ̄39Ar ctating
Lost rate of  ̄39Ar
Tieling Formation
Jingeryu Formation