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Common reflection surface(CRS) stack is a macro-model independent seismic imaging method. 共反射面元 (commonreflectionsurface ;CRS)叠加是一种不依赖于宏观速度模型的零炮检距剖面成像方法 .
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。
Common Reflection Surface(CRS) stack,a new stacking technique compared with conventional common midpoint(CMP) stack,is a zero-offset profile imaging method independent of macro-model. 共反射面元(CRS)叠加与常规共中心点(CMP)叠加相比是一种崭新的叠加方法。它是一种不依赖于宏观速度模型的零炮检距剖面成像方法,它的实现只依赖于3个波场属性参数的确定。
Common Reflection Surface (CRS) stack 共反射面元（CRS）叠加
common reflection surface(CRS) stack 共反射面元叠加
Common reflection surface stack algorithm and processing flow 共反射面元叠加的实现途径及流程
A method of dip decomposition common reflection surface stack 倾角分解共反射面元叠加方法
AN APPLIED THEORY ON COMMON REFLECTION SURFACE STACK--FROM COMMON REFLECTION POINT TO COMMON REFLECTION SURFACE 共反射面元叠加的应用理论--从共反射点到共反射面元
Application of attribute parameter of common reflection surface (CRS) stack wave field 共反射面元叠加波场属性参数的应用
Keywords Common Reflection Surface （CRS） stack;Attributes;Data-driven;Simplex method;Optimization.; 共反射面元（CRS）叠加;属性参数;数据驱动;单纯形法;最优化;
common reflection surface 共反射面元
common reflection surface stack 共反射面叠加
It not only includes the characteristic of low PDL, but also can be easily fabricated compared to the common reflection type VOA. 此设计不仅有反射式光衰减器的低偏极相关损耗(PDL)的优点，而且相较于一般的反射式光衰减器其制作上非常简单。
Like common depth point, this term is commonly misused, because in the case of dipping layers, common reflection points do not exist. 如同共深度点一样，该术语也通常被误用，因为在倾斜层的情况下，并不存在共反射点。
Reasonable reflective surface, soft light, glareproof, uniform brightness. 合理的反光曲面，光线柔和，无眩光，光亮度均匀。
Pairs of such reflecting surfaces are known as etalons. 这样一对反射面通常称为标准具。
Knowledge without common sense counts for little. 光有学问而无常识，则这种学问无甚价值。
As the common mid-point (CMP) stacking is hard to get a good effect in the complicated geological structure in seismic data processing, the common reflection point(CRP) stacking is used. 在地震勘探数据处理中,通常采用的共中心点(CMP)叠加技术对于复杂的地质构造难以取得好的效果。
The light wave that has bounced off the reflecting surface is called thereflected ray. 从反射表面跳回的光波称为反射线。
AVO inversion is an important aspect of its techniques which is to make inversion for the varieties of amplitude versus offset based on the normal pre-stack common reflection gathering and extract compressional wave, shear wave and density. AVO反演是AVO技术的重要组成部分,它是对常规叠前共反射点道集的振幅随炮检距变化进行反演,提取纵、横波速度和密度,AVO反演不同于其它地震反演。