The fine seismic reinterpretation is conducted on the Southern Slope by establishing a seismic interpretation for the discovered reef flat facies in the Northern Slope of the Tazhong Uplift.

• 建立塔中北坡已发现礁滩相的地震解释模型,对南坡地震资料重新进行了精细解释,识别出塔中隆起南部斜坡具有与塔中隆起北坡相似的坡折带地震反射特征,发育大型台地边缘礁滩相沉积;