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福建省石炭系主要分布于闽西南永梅拗陷,北至将乐、南平,东到德化、安溪,西南与江西、广东相接,此外闽东北的福鼎南溪也有出露,其沉积范围共约4.2万平方公里,占全省总面积的1/3左右。按岩性组合及生物群特征自下而上可分为下统林地组、中统黄龙组、上统船山组*_1。(表1),从岩性、岩相及生物区系来看,与华南其他地区应属同一海盆,并大致可以对比(表2附图)。
The Carboniferous of Fujian Province is mainly distributed in the Yongmei Depression in the southwest of Fujian Province. In the north, there will be music, Nanping, east to Dehua, Anxi, southwest and Jiangxi and Guangdong. In addition, Fuding Nanxi in northeast Fujian is also exposed, A total area of about 42,000 square kilometers, accounting for about 1/3 of the total area of the province. According to the characteristics of lithology and biota, it can be divided into the lower forest group, the Central Huanglong Formation and the upper Chuanshan Formation * _1. (Table 1). From the perspective of lithology, lithofacies and biota, it should belong to the same basin as the rest of South China and can be roughly compared (Table 2 attached).