| 1. | Seismic wave field modeling with convolutional differentiator algorithm
地震波场模拟中的褶积微分算子法 |
| 2. | Input seismic wave fields in elastic half - space interbedded by liquid - filled porous medium and solid medium
不同介质互层分布的弹性半空间地震波场输入 |
| 3. | In this pa per , field seismic wavefields were simulated with seismic physical modeling technique
利用地震物理模拟技术在实验室内再现了野外观测到的复杂地震波场。 |
| 4. | In resent years , a lot of researches of seismic required of complex medium have been done home and abroad
面对这种发展趋势，近年来国内外有关学者进行了大量的复杂介质地震波场研究。 |
| 5. | The complex seismic wavefield beneath high velocity layer was investigated on layer stripping observations of seismic physical model
通过地震物理模型的分层观测，详细研究了高速屏蔽层下的复杂地震波场。 |
| 6. | In this thesis , the characteristics of wavefield in orthotropy media was investigated by means of seismic physics model technique
本文利用地震物理模型正演技术，开展正交各向异性介质地震波场特征的研究。 |
| 7. | Finally , in term of the analysis the characteristic of the seismic wavefield of fractural reservoir , the paper adopts the numerical simulation
最后，为了分析出缝洞储层地震波场的地震波场的特点，本文采用了数值模拟的方法。 |
| 8. | It is significant for energy exploration , seismic prospecting , groundwater utilized and rock engineering to study the characteristics of seismic wavefields in those orthotropy media
研究正交各向异性介质中地震波场特征对地震预测、岩体工程、地下水利用和能源勘探开发有十分重要的意义。 |
| 9. | Common reflection surface ( crs ) stack , which depends on three attributes of the seismic wave - field , is a seismic imaging method independent of the macro - model
摘要共反射面叠加方法运用3个地震波场参数来描述地下反射面元时距关系，不对地下反射界面形状做任何假设，并且是一种不依赖于宏观速度模型的反射波成像方法。 |
| 10. | The paper deduced movement and wave equation of seismic wave field in constant q viscoelastic media using the method of pseudo - spectral , and carried on forward modeling , the modeling result is the same with the one of other modeling ways
摘要本文采用伪谱法推导了常q粘弹介质中地震波场的运动方程和波动方程，并进行了地震波场数值正演模拟，模拟结果达到了其它模拟方法同样的效果。 |
