邢台震区近场观测的启示 1966年邢台地震开创了我国近代地震研究的新局面。我们做为邢台地震老战士,与同事们一起,采用当时国内精度较高的钢弦式钻孔应力仪,日日夜夜“为党中央站岗,为工农兵放哨”。在深入现场的过程中,观测到许多至今仍被国内外同行所重视的地震近场信息。邢台震区属华北沉陷区地震带,区内自新生代以来强烈下沉,被第四系所覆盖。震区有三处基岩出露,即荒山、卧牛山(后改名红山)和茅山。我们的研究工作,从一开始就在李四光教授指导下进行的,他多次听取仪器研制方 Enlightenment of near field observation in Xingtai earthquake area The 1966 Xingtai earthquake created a new situation in the research of modern earthquake in our country. As an old soldier of the Xingtai earthquake, together with our colleagues, we used the steel string-type stress gauges of high precision at that time in our country to “stand guard for the party Central Committee and guard the workers, peasants and soldiers” day and night. In the process of going deep into the field, many near-field earthquakes that are still valued by domestic and foreign counterparts are observed. The Xingtai earthquake zone belongs to the seismic zone in the subsidence area of ​​North China. The area has been strongly subsided since the Cenozoic and covered by Quaternary. There are three earthquake bedrock exposed, that is, barren hills, lying Niu Shan (later renamed Hongshan) and Maoshan. Our research work, under the guidance of Professor Li Siguang from the very beginning, he repeatedly listened to the instrument development side