Layering method suitable for shallow stratum layer of sedimentation basin
A stratigraphic and shallow layer technology, applied in seismology, geophysical measurement, seismic signal processing, etc., can solve the problems of inability to generate reflected wave events, increase the difficulty of ore-forming target layers, and increase the blind area of reflected wave exploration, etc.
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Embodiment 1
[0017] The present invention comprises the following steps in turn:
[0018] Step 1: When the total depth of the stratum to be stratified is less than 50 meters, use seismic waves to extract the dispersion curve of seismic waves; the detection conditions are: 12 seismic acquisition channels, 20 Hz geophone frequency, 5 meters offset distance, and 1 channel spacing 1 meter, sampling rate 0.5 milliseconds, recording length 1 second, end-point excitation, well depth 3 meters, charge 1 kg; along the survey line, conduct field measurements at a fixed shot spacing of 5 meters;
[0019] Through the extraction of the seismic wave dispersion curve, the density and compressional wave velocity of the formation within the detection range are inverted;
[0020] The second step is to obtain the wave impedance parameter, which is the density (ton / m 3 ) and the product of the longitudinal wave velocity (m / s);
[0021] The third step is to select the lowest value of the wave impedance parame...
Embodiment 2
[0023] The present invention comprises the following steps in turn:
[0024] The first step, when the total depth of the stratum to be stratified is 50 meters to 100 meters, use the seismic wave to extract the dispersion curve of the seismic wave; the detection conditions are: 48 seismic acquisition channels, the receiver frequency is 10 Hz, and the offset distance is 10 meters , the track spacing is 5 meters, the sampling rate is 1 millisecond, the recording length is 2 seconds, the end point is excited, the well depth is 4 meters, and the dose is 2 kilograms; along the survey line, the field measurement is carried out according to the fixed shot spacing of 10 meters;
[0025] Inversion of the density and compressional wave velocity of the formation within the detection range through the dispersion curve of the seismic wave;
[0026] The second step is to obtain the wave impedance parameter, which is the density (ton / m 3 ) and the product of the longitudinal wave velocity (m...
Embodiment 3
[0029] The present invention comprises the following steps in turn:
[0030] The first step, when the total depth of the stratum to be stratified is 100 meters to 150 meters, use the seismic wave to extract the dispersion curve of the seismic wave; the detection conditions are: the seismic acquisition channel is 96 channels, the receiver frequency is 4Hz, and the offset distance is 30 meters , the track spacing is 10 meters, the sampling rate is 2 milliseconds, the recording length is 2 seconds, the endpoint is excited, the well depth is 10 meters, and the charge is 2 kilograms; along the survey line, the field measurement is carried out according to a fixed shot spacing of 50 meters;
[0031] Inversion of the density and compressional wave velocity of the formation within the detection range through the dispersion curve of the seismic body wave;
[0032] The second step is to obtain the wave impedance parameter, which is the density (ton / m 3 ) and the product of the longitud...
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