沉积相揭示了目的层段的沉积环境、储集岩成因及其分布规律。
Sediment facies reveal the sediment environment of the interest interval, the origin and distribution rule of the reservoir.
在地震资料处理过程中，为了提高目的层段反射同相轴的分辨率，通常采用反褶积的方法。
Deconvolution has been usually adopted in the process of seismic data processing in order to improve resolution in reflection event of objective interval.
为此，要想在该区上第三系目的层段优选有利目标，必须对其进行精细构造解释和储层预测。
Therefore, if good objects are going to be chosen in zones of palaeogene, the fine tectonic interpretation and reservoir prediction must be needed.
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