低信噪比复杂断块区地震资料解释

2004年 11卷 第02期
阅读:108
查看详情
The Seismic Data Interpretation of Low SNR Complicated Fault Block Area in Tabei Region of the Subei Basin


陈忠慰1 陈忠云2 崔永福2
1.中国石化西部勘探指挥部 2. 石油大学资源与信息学院,北京
地震资料低信噪比一直是影响地震解释方案可靠性的主要因素之一。以塔北低信噪比复杂断块区为例,研究低信噪比复杂断块区的解释思路和方法。该区地下地层破碎,断裂复杂,地震资料的信噪比总体较低,主要表现为:地震反射不连续,反射能量弱; T31 地震反
射特征可对比性差,T33 反射特征横向有变化;断面及断点反射不清;具多产状干扰。针对这些问题,提出了相应的解决对策,主要做了速度分析、全三维解释、深度校正等研究,基本上解决了地层层位的落实和断层识别这2 个在复杂断块区地震资料解释中所要解决的主要问题。通过对塔北低信噪比复杂断块区的地震资料解释,落实了塔8 反向断鼻构造,并通过了井位论证,实钻,塔x8 井在E1f2地层见良好油气显示。
The low SNR of seismic data is one of the main factors
that work on the reliability of seismic interpretation. The
complicated fault block area with low SNR in Tabei region of
the Subei Basin is a good example to study and sum up the
interpreting methods in the complicated fault block area.
The feature of Tabei region of the Subei Basin includes
underground rock disintegration , complicated fault block ,
the general low SNR. There comes forth four obvious
problems when carrying out seismic interpretation : 1. the
discontinuity and the weak energy of seismic reflection ; 2.
the bad comparability of the T13reflectance signature and
transverse variety of T33
reflectance signature ;3. the unclarity
of fault surface and breakpoint ; 4. the disturbance of multi2
attitude. Aiming at the above problems , applying the
corresponding countermeasures such as velocity analysis , full
3-D interpretation and depth correction , the two basic
questions of the identification of stratigraphic horizons and
the detection of faults were basically solved. Both questions
are the main tough problems during the seismic data
interpretation. After the seismic interpretation of low SNR
complicated fault block area in Tabei region of the Subei
Basin , the Ta-8 reverse nose structure was identified and
well location demonstration was passed. And the real drilling
illustrates the favorable evidences of oil and gas in the E1 f2
layer of well Ta-8.


信噪比; 层位标定; 地震反射特征;
SNR , Horizon demarcation , Seismic reflectance signature.


;