表层地震断层探测方法应用研究  

On the Detection Means For Shallow Earthquake Fault

作　　者：吴子泉[1] 盖殿广[2] 王成虎[1] 王振强[2] 

机构地区：[1]中国地质大学,北京100083 [2]山东省地震局,山东济南250014

出　　处：《土工基础》2005年第1期57-60,共4页Soil Engineering and Foundation

摘　　要：根据地表下埋深 10米断层的探地雷达和地震映像探测资料 ,讨论了超浅层地质构造的探测方法。认为地震映像因干扰信号强、不能定量解释等缺点 ,建议不单独使用 ;探地雷达方法可适当使用 ,但勘探深度不宜超过 2Based on the detection data of geological radar and seismic map for the underground faults at the 10 m depth, this paper discusses the detecting means for the super-shallow geological structures. It is considered that the seismic mapping means shall not be used alone due to its disadvantages of strong disturbance signals and non-quantitative interpretation. The geological radar means can be used properly to some extent, but the exploration depth shall not exceed 20 m.

关 键 词：地震断层 探测方法 定量解释 勘探深度 表层 探地雷达 探测资料 地质构造 地表 埋深 

分 类 号：TU564.6[建筑科学—建筑技术科学] P631[天文地球—地质矿产勘探]