摘要
Based on a sample of some real earthquakes,we have suggested in previous papers that there is a density-tectonic stress wave with ultra-low frequency which is emitted from the epicenter region for months before earthquakes,and a micro-fracture wave 1 ～ 10 days before earthquakes. The former has been observed by different kinds of measurements and the latter has been observed by a few chance observations which consists of electromagnetic,gravitational and sonic fluctuations. We show real observational results that depict the two waves and they have very different frequencies,which are not difficult to discriminate. The classical elastic-rebound model is one of the most influential theories on earthquakes,and the thermodynamic elastic-rebound model has amended the classical framework. Considering the two waves above,we attempt to further modify the elasticrebound model,and the new framework could be called the "micro-fracture elasticrebound model". We infer that tectonic earthquakes could have three special phases: the accumulation of tectonic stress,micro-fracture,and main-fracture. Accordingly,there would be three waves which come from the epicenter of a tectonic earthquake,i. e. ,the tectonic stress wave with ultra-low frequency a few months before the earthquake,the micro-fracture wave about 1 ～ 10 days before the earthquake and the main-fracture wave (common earthquake wave).
Based on a sample of some real earthquakes, we have suggested in previous papers that there is a density-tectonic stress wave with ultra-low frequency which is emitted from the epicenter region for months before earthquakes, and a micro-fracture wave 1 ~ 10 days before earthquakes. The former has been observed by different kinds of measurements and the latter has been observed by a few chance observations which consists of electromagnetic, gravitational and sonic fluctuations. We show real observational results that depict the two waves and they have very different frequencies, which are not difficult to discriminate. The classical elastic-rebound model is one of the most influential theories on earthquakes, and the thermodynamic elastic-rebound model has amended the classical framework. Considering the two waves above, we attempt to further modify the elastic- rebound model, and the new framework could be called the ＂ micro-fracture elastic- rebound model＂. We infer that tectonic earthquakes could have three special phases： the accumulation of tectonic stress, micro-fracture, and main-fracture. Accordingly, there would be three waves which come from the epicenter of a tectonic earthquake, i. e. , the tectonic stress wave with ultra-low frequency a few months before the earthquake, the micro-fracture wave about 1 ~ 10 days before the earthquake and the main-fracture wave （common earthquake wave）.
