一、福建海平面升降简况本文是作者自1931年到现在,从事研究福建海平面升降运动的回顾和总结。作者于1931年在平潭岛上见到小海湾、海积、海蚀阶地、洞穴等均有抬升,在四十年代一些地质工作者相继提出华南海岸上升的论点。作者认为福建海岸格局深受新华夏系断裂构造的控制。同时也受到北西和东西向构造的切割,这些断块有升有降,升降不等的断块,刻划了锐利破碎曲 First, the Fujian sea level lift profile This article is from 1931 to now, the author engaged in the study of Fujian sea level movements in the review and summary. In 1931, on the island of Pingtan Island, the author saw small coves, and the sea area, sea-catenary terraces and caves were all raised. In the forties, some geologists came up with the argument that the south China coast should rise. The author believes that the coastal pattern of Fujian is well controlled by the fault structure of the New China. But also by the North West and east-west structure of the cut, these blocks have ups and downs, lift up and down the block, scratched sharp broken song