摘要
利用浅层地震勘探对广东龙川东江老隆大桥桥址进行勘查 ,得到测区基岩面的起伏形态、速度分布以及断层位置。结果表明 ,测区为一条近南北向的断裂沉降带 ,桥址的中心线正好通过其中。从经济与安全的角度出发 。
The prospecting results showed the bedrock interface feature、its velocity structure and fault location. The results also indicat that there is a belt of subside rupture running through the central line of the bridge.So that it is better to reselecte the bridge site in the view point of economy and safety consideration.
出处
《华南地震》
1998年第4期74-77,共4页
South China Journal of Seismology
关键词
地震勘探
地震波折
基岩
断裂沉降带
桥址
桥
Seismic exploration,Seismic refraction method,Bedrock,Fault subsidence zone