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不同类型盆地的层序充填样式、展布特征存在较大差异。前陆盆地的层序发育主要受控于逆冲挠曲变形和负载释放的交替作用，层序展布上表现为极度的不对称；克拉通盆地因地形平坦，海平面升降对层序发育起主要控制作用，层序特征在较大的范围内表现出很好的一致性；断裂不同规模、不同级次的幕式活动控制了陆内裂谷盆地层序各级次旋回的发育，因此，盆地层序往往具有多级旋回的特征；大型坳陷盆地由于水体广阔，层序特征可与被动陆缘类比；山间坳陷盆地的层序发育主要受幕式构造活动、古气候以及物源等因素的影响；山前断陷盆地的层序发育则主要受走滑拉分作用的控制。上述这些差异必然会导致不同盆地的生储盖类型及其配置关系有较大差别。就一般而言，各级次旋回中由上升到下降的转换位置是烃源岩发育的位置；上升半旋回和下降半旋回中形成的各类砂体是主要的储集体。
Different types of basin sequence filling pattern, distribution characteristics are quite different. The sequence development of the foreland basin is mainly controlled by the alternation of thrust deflection and load release, and the sequence distribution is extremely asymmetric. Due to the flat topography and the sea level rise and fall, the sequence stratigraphy develops in the craton basin The main control and sequence features show good consistency in a wide range. The episodic activities of different scales and different levels of fracture control the development of the secondary cycles at all levels in the intracontinental rift basin. Therefore, The sequence of the basins in the basin is often characterized by multistage cycles. Because of the vast body of water in the large depression basins, the sequence features can be compared with the passive margins. The sequence development of the depression basins in the depression is mainly affected by the tectonic activity, paleoclimate and source And other factors. The sequence development of the Piedmont rift basin is mainly controlled by the function of the slippage and pull points. These differences will inevitably lead to different types of reservoirs and their distribution in different basins. Generally speaking, the position of source rock development is from the ascending to the descending transition position in all levels of cycles. The various types of sand bodies formed during the ascending half-cycles and descending half cycles are the main reservoirs.