北部湾盆地在中始新世至早渐新世是一个湖泊。
Beibu Wan Basin was a lake in the middle Eocence-Lower Oligocene.
在系统分析北部湾盆地涠西勘查区地震剖面的基础上，认为北部湾盆地涠西勘查区发育两期反转构造即渐新世末期及中新世末期反转构造。
It was indicated that there were two different inversion structures formed in two period based on analysis of seismic profiles in Weixi exploration region of the Beibuwan Basin.
海南地体运动规律的阐明对于了解北部湾油气盆地的形成演化有重要的理论和实际意义。
Elucidation of the law of movement of Hainan Terrane has great theoretical and practical significance for study on the formation and evolution of the oil and gas basins in Beibu Gulf.
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