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福建省以山地丘陵居多,平原狭小,除了分布于山区的山间盆地以外,多数位于沿海一带。规模较大的有福州盆地,漳州盆地,龙海盆地,泉州盆地,蒲田平原,长乐平原等第四纪盆地或槽地。它们都形成于第四纪,是新构造运动以来地壳受多组活动断裂的切割,发生断块差异运动的产物(图1)。据区域地质的研究,闽省沿海东邻台湾海狭
Mostly in Fujian Province, mountainous hills, small plains, in addition to distributed in mountainous mountain basin, the majority are located in the coastal areas. The larger Fuzhou Basin, Zhangzhou Basin, Longhai Basin, Quanzhou Basin, Kamata Plain, Changle Plains and other Quaternary basins or trough. They were all formed in the Quaternary. They are the result of the cutting of the crust by multiple active faults since the Neotectonic Movement and the differential motion of the fault blocks occurred (Figure 1). According to regional geological research, coastal province of Fujian Province, east of Taiwan Sea narrow