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| 表层地震断层探测方法应用研究 | |
| 引用本文： | 吴子泉,盖殿广,王成虎,王振强.表层地震断层探测方法应用研究[J].土工基础,2005,19(1):57-60. |
| 作者姓名： | 吴子泉 盖殿广 王成虎 王振强 |
| 作者单位： | 1. 中国地质大学,北京,100083;山东省地震局,山东,济南,250014 2. 山东省地震局,山东,济南,250014 3. 中国地质大学,北京,100083 |
| 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 2 0米 |
| 关 键 词： | 地质雷达 地震映像 定量解释 |
| 文章编号： | 1004-3152(2005)01-0057-04 |
| 修稿时间： | 2004年3月15日 |
On the Detection Means For Shallow Earthquake Fault |
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| WU Zi-quan{,},GAI Dian-guang,WANG Cheng-hu,WANG Zhen-qiang.Chinese Geology Univ,Beising, .Shandong Bureau of Seismoloy,Jinan,China.On the Detection Means For Shallow Earthquake Fault[J].Soie Engineering and Foundation,2005,19(1):57-60. | |
| Authors: | WU Zi-quan{ } GAI Dian-guang WANG Cheng-hu WANG Zhen-qiangChinese Geology Univ Beising Shandong Bureau of Seismoloy Jinan China |
| Affiliation: | WU Zi-quan+{1,2},GAI Dian-guang+2,WANG Cheng-hu+1,WANG Zhen-qiang+21.Chinese Geology Univ,Beising,100083, 2.Shandong Bureau of Seismoloy,Jinan,250014,China) |
| Abstract: | Based 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. |
| Keywords: | geological radar seismic mapping quantitative interpretation |
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