确定断层位移速度,计算构造脉动和强热地震的重复率,在地震地质和地震学研究中具有越来越重要的意义,它是制定长期预报地震领域的基础。在确定1000—10000年前地质和地震事件年代时,首先应当采用放射性碳同位素和考古方法。本文研究了用这些方法确定中亚 It is more and more important to study the seismic geology and seismology to determine the fault displacement velocity and calculate the repetition rate of tectonic pulsation and intense thermal earthquake. It is the basis for making long-term prediction of the earthquake field. In determining the years of geological and seismic events 1000-10000 years ago, radioactive carbon isotopes and archeological methods should first be used. This paper studies the use of these methods to determine Central Asia