Based on the view, combining actual seismic data ,the author draws the conclusion that the lower—limit magnitude of strong earthquake is 7.1 in Chinese Continent ,and the thickness of seismogenic layer is 20km.
The paper first discusses the methods of fractal, fractal dimension, random fractal interpolation and then applies them to the actual seismic data processing.
We may describe seismic facies conti- nuity and change of amplitude and frequency by S-Trans- form seismic facies analysis of the ideal seismic sequence model and actual seismic data.
The conception of transient frequency and calculation method of wavelet packet are introduced,and time frequency distribution about simulation and actual seismic signals is given.
The model parameters can be applied in actual seismic inversion directly,and it will provide instruction to improve accuracy and reliability for effective reservoir prediction.
By replacing the basic wavelet in the ST with actual seismic wavelet which was extracted from seismic data, the general S transform (GST) was achieved in the seismic data analysis.
It formalizes an approximate inversion method which is based on the interpretation of local inhomogeneities as making the differences between an actual seismic data set and a previous reference model.
On the basis of simulated wavelet, a processing method for eliminating deconvolution and changing wavelet is put forward in this paper. The processing method for eliminating deconvolution can decompose a seismic wave train into a series of apparent seismic wavelets, which, having undergone changing wavelet proeessing, becomes a new seismogram. This method does play an obvious role in improving seismic wave resolution and advancing velocity accuracy. The kinematic and dynamic informations o...
In the case of uniform medium, seismic wave is considered as a sinusoidal pulse, but in non-uniform medium, it can be expressed by Fourier series or Fourier integral. According to this knowledge, we can obtain required residual abnormal traces (residual waveform) by first simulating normal reflection with symmetric sinusoidal pulse then substracting weighted sinusoid record from actual seismic record. The residual abnormal traces can be used for identifying special lithology and geologic s...
This paper points out the mistake occurring in studying seismic wave by optical method and analyses the current migration theory and methods. It is pointed out that in the consideration of single secondary source, the reverse wave motion Huygens' principle can be thought right, while taking it as sole migrating principle is wrong. It is inappropriate to sum up and explain all kinds of migration method by "generalized diffraction transform method" based on the single secondary source. The acknowledgmen...