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1.Fitting the zero-offset reflection record by AVO principle.
利用AVO原理拟合炮检距道反射记录收藏指正
2.Calculating the Zero Offset P and S R eflection Using the Nnoe-Zero Offset P-P and P-SV Wave
用非偏P-P波、P-SV波计算偏反射纵波和反射横波收藏指正
3.Fitting a zero-offset seismic trace in time-frequency domain.
时频域炮检距地震道拟合收藏指正
4.In the paper, according to the theory that the resolution of each seismic trace in common midpoint (CMP) gather can be reduced along with the increase in offset, the cause of forming dynamic correction stretching is explained and the stretching factor of the non-zero offset trace relative to the zero offset trace is derived in light of the generalized resolution formula.
文章以共中心点道集中各地震道分辨率随炮检距增大而降低为理论依据,说明动校正拉伸的形成原因,并且根据广义分辨率公式导出了非炮检距各地震道相对于炮检距地震道的拉伸因子。收藏指正
5.Zero offset(ZO) section, which is just the goal of CMP stacking in conventional processing, is an important intermediate result in seismic reflection imaging.
炮检距剖面是地震反射成像过程中重要的中间成果 ,常规处理中的共中心点 (CMP)叠加的目的正在于此。收藏指正
6.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。收藏指正
7.Based on analyzing AVO characters of seismic CMP gather and stratigraphic absorption passing different path by different offset signal,the paper discovered that for different frequency component of seismic signal at different offset signal at a certain moment,the relation between frequency and offset x can be described by polynomial and then the technique of fitting a zero offset seismic trace in time frequency domain based on time frequency analysis and fitting of polynomials has been proposed.
本文在分析地震共中心点道集的 AVO特性 ,以及不同炮检距信号经过不同路径的地层吸收的基础上 ,发现对于某一时刻的不同炮检距地震信号的不同频率成分 ,可以用多项式描述其与炮检距 x的关系 ,进而提出了基于信号时频分析和多项式拟合的时频域炮检距地震道拟合技术。收藏指正
8.Based on the similarity of common reflection point trace gathers in one coherent zone, CRS stack can focus more energy on the vicinity of the reflector, and therefore can obtain a high signal-to-noise ratio zero offset section by stacking events with the same phase.
共反射面叠加利用了邻近多个共反射点道集的相似性,提高了资料的覆盖次数,从而压制了随机噪声,增强反射波同相轴的连续性,大幅提高了地震资料的信噪比。收藏指正
9.To perform CRS stack depends on the determination of three wave attributes,compared with conventional common middle point(CMP) stack and dip move out(DMO) stack,CRS stack can focus more energy in the vicinity of the reflector,therefore can obtain a better zero offset section by stacking events with same phase.
共反射面元的旅行时响应由三个波场属性参数确定 ,相比常规共中心点 (commonmiddlepoin ,CMP)叠加和倾角时差校正 (dipmoveout,DMO)叠加 ,CRS叠加算子能够将地下反射点附近一个邻域内的能量进行聚焦并实现同相叠加 ,因此能得到更好的炮检距剖面 .收藏指正
10.Metrological Atomic Force Microscope with Zero Abbe Offset
阿贝误差计量型原子力显微镜收藏指正
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