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地球物理勘探二维弹性波传播有限差分数值模拟-Geophysical two-dimensional finite difference elastic wave propagation simulation
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用二阶有限差分法的中心差分格式来模拟二维均匀介质中声波传播，震源子波是雷克子波-Finite difference method with second order central difference scheme to simulate two-dimensional wave propagation in uniform media, the source wavelet is a Ricker wave
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用有限差分法的四阶差分格式模拟声波在二维均匀介质中的传播，不带吸收边界条件，震波是雷克子波-Finite difference method of fourth order difference scheme for two-dimensional simulation of acoustic wave propagation in uniform medium, without absorbing boundary condition, shock wave is Ricker
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二维声波数值模拟正演程序，利用有限差分法，没有加入吸收边界-Numerical simulation of two-dimensional acoustic forward procedure, using the finite difference method, did not join absorbing boundary
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勘探地震学 研一课程 二维速度结构的时域有限差分模拟 采用雷克子波-Exploration seismology Kenichi course of the two-dimensional velocity structure using finite difference time domain simulation Ricker wave
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