摘要
本文阐述了主要利用关中活断层中的断层泥进行热释光年龄测定的方法和步骤，得出了１４个数据，比较了一些具有地层层位的数据与用断层坎扩散方程计算出的结果，证明这些数据与用断层坎扩散方程计算出的结果大约有５ ％ ～１０％ 或稍大的误差。从科学发展的现阶段看，这些结果是可信和可用的，关中活断层在２ ～１６－５
The methodgeo of thermoluminescence, dating by mainly using the gouge of active fallts in the Guanzhong area of Shaanxi province is mainly introduced Forteen dating ages have been given By comparison of some obtained date with its stratigraphic position and with the caculation result of fault scarp by using diffusion equation, it is showed that the data have an error about 5%10% or some more They are reliable and feasible in the present stage of science development The results also shows that the active faults in the researched region have been brished during 20165 KaBp [
出处
《地球科学与环境学报》
CAS
1999年第S1期77-79,82,共4页
Journal of Earth Sciences and Environment
关键词
活断层
热释光
陕西关中
active faults, thermoluminescence, Guanzhong of Shaanxi
