【摘 要】
：
埕岛地区馆上段为一套曲流河冲积平原沉积，其砂岩储层单层厚度小，横向变化大。针对这件特点，本文尝试使用地震岩性方法，利用多件地震信息，包括合成地震记录、频率和展速度分析、道
【机 构】
：
胜利石油管理局地质科学研究院,胜利石油管理局地质科学研究院,胜利石油管理局地质科学研究院
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埕岛地区馆上段为一套曲流河冲积平原沉积，其砂岩储层单层厚度小，横向变化大。针对这件特点，本文尝试使用地震岩性方法，利用多件地震信息，包括合成地震记录、频率和展速度分析、道积分利面、GLOG剖面，对埕岛地区馆上段储层分布进行解释和预测。
The upper section of Chengdao area is a set of meandering alluvial plain sediments. The thickness of sandstone reservoir monolayer is small and lateral variation is large. In response to this feature, this paper attempts to use the seismic lithology method to interpret the reservoir distribution in the upper part of the Chengdao area using multiple pieces of seismic information, including synthetic seismograms, frequency and spreading velocity analysis, channel integral facets, and GLOG profiles prediction.
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