万安盆地是南海西南部陆架上的大型新生代沉积盆地。
Wan 'an basin is a large scale Cenozoic sedimentary basin which is located on southwest shelf of the south China Sea.
根据基底性质分析，探讨了东海大陆边缘新生代沉积盆地的形成演化与成因机制。
Along the continental margin in East China Sea, the origin and evolution of Tertiary sedimentary basins are discussed, based on analyses of basement nature.
南海地区新生代沉积盆地有四类：张裂盆地、走滑拉张盆地、前陆盆地和前弧盆地。
There have four kind of basins in the South China Sea area: rifting basin, strike-slip rifting basin, fore-land basin and fore-arc basin.
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