摘要
本文根据野外实际调查,参考前人成果,研究了福建海岸地区断裂构造特征及其应用。结果表明,福建海岸存在着E-W、S-N、NE、NNE和NW向五组断裂带,其中明显的断裂有40条。这五组断裂生成先后顺序大致为:E-W、S-N、NE、NNE、NW向,它们既控制了福建海岸的形成与发育,也为沿海地区找矿、港口开发、地震预测、水文地质和工程地质工作提供了重要标志。
This paper studies the fault structural characteristics and its practical significance in the coastal area of Fujian province,according to the data of our on-the-spot field investigations,consulting previous studied results.Our study indicates that there are five groups of faults in this area.They formed in the temporal sequence from E-W to S-N,NE,NNE and then to NW.Among them,40 faults are obvious.The faults control the formation and development of Fujian coast and serve as an important factor in mineral discovery,port exploitation,earthquake prediction hydrogeology and engineering geology in the coastal area.
作者
陈峰
Chen Feng(Third Institute of Oceanography,SOA,Xiamen)
出处
《台湾海峡》
CAS
1988年第3期65-71,共7页
Journal of Oceanography In Taiwan Strait
