作　　者： ; ; (黎烈均）;

机构地区： 中山大学地球科学系地质系

出　　处： 《中山大学学报论丛》 1992年第1期104-110,共7页

摘　　要： 探讨了热释光测定断层最新活动年代的理论和方法,以及测年数据普遍偏老的原因。 Based on authors study for many years. The chievements in the scientific studies on the theory and the technique of the thermoluminescent dating for the fault movements have been sum up in this paper. It is put forward by the authors that the samples which are used for TL dating, are selected from the materials in the fault slipping surface and adhered it, and then, the degree of accuracy for the ages of the fault movement by the TL dating is improved. This method may be the way to determine the ages of the fault movement since Holocene.

关 键 词： 断层物质 矿物热释光增长非线性 断层滑动面

领　　域： [文化科学] [文化科学]