摘要
Using the methods of subordinate function, variation rate and trend rate, the authors extract the earthquake precursory anomalies from observational data of Radon in southeastern Gansu Province. The result indicates that 7 items of radon data include 47 subordinate-function anomalies, 45 variation-rate anomalies and 39 trend-rate anomalies from January 1984 to December 2009. Among them, 33 subordinate-function anomalies, 35 variation-rate anomalies and 30 trend-rate anomalies corresponded with the earthquakes MS5-8 that ever hit Gansu Province and the adjacent region within 33 to 585 km. By the analysis of the features of these anomaies and their relation to the earthquakes, the method of time prediction for the moderate-strong and strong earthquake were proposed, and the empirical constant, variation rate and threshold value of trend-rate anomaly are obtained from Radon in southeastern Gansu Province.