Three-dimensional fault-dissolved body model making method
A production method and three-dimensional technology, applied in geographic modeling, measuring devices, instruments, etc., can solve problems such as difficult to identify outer bands, frequency reduction, amplitude weakening, etc.
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[0026] 1. The method for making a model of a three-dimensional fault-karst body comprises the following detailed steps in turn:
[0027] Step 1: Obtain the layer velocity of overlying stratum 1 and overlying stratum 2, destination overlying strata, fault dissolution zone, dissolution fracture-cavity system, compact limestone, compact limestone 1, and compact limestone 2 respectively, according to Gardner The formula calculates the density, and the wave impedance is calculated from the velocity and density.
[0028] Gardner's formula: ρ=0.31*v 1 / 4 ;
[0029] ρ is the density of the rock mass in this layer, and v is the wave velocity of the rock mass in this layer.
[0030] Wave impedance formula: δ=ρ*v;
[0031] δ is the wave impedance of the rock mass in this layer.
[0032] Step 2: Involved seismic parameters: wavelet frequency is 30Hz.
[0033] Step 3: According to the schematic diagram, first draw a two-dimensional fault-karst body velocity, density, and wave impedance...
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