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The detection of buried faults in engineering sites and the evaluation of seismic activity |
Ming-Hui LIU1, Jian XUE2, Zhe-Jiang WANG2, Yuan-Xin WANG2, Wen-Bin SHEN1 |
1. The Sixth Geological Survey of Jilin Province, Yanji 133001, China 2. College of Earth Sciences, Jilin University, Changchun 130026, China |
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Abstract The geological exploration methods for geological faults include shallow seismic exploration, electrical joint section method, resistivity sounding, electrical resistivity tomography, geological radar and transient electromagnetic method. The distribution of geological structure can be detected from the velocity and relative permitivity. From the distribution of activities of faults, geological data, remote sensing data and isotope or thermoluminescence dating techniques, a scientific evaluation can be made. The above research would be important for the rational use of the site and the safety of the layout of the project. In this paper, the geophysical prospecting of a cement production line in Changchun serves as an example to discuss the exploration and activity evaluation of geophysical methods for concealed ruptures.
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Received: 06 April 2017
Published: 03 August 2018
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样品名称 | 样品编号 | 年龄/104a | 备注 | 黑灰色含角砾亚黏土 | C1-1TL | 10.48±0.82 | F1断层盖层 | 灰白色含角砾亚黏土 | C1-2TL | 13.07±1.02 | F1断层盖层 | 巧克力色黏土 | C2-1TL | 10.58±0.89 | F2断层盖层 | 黑灰色黏土 | C2-2TL | 25.71±1.98 | F2断层盖层 | 米黄色亚黏土 | C2-3TL | 26.98±2.16 | F2断层盖层 | 断层泥 | C2-4TL | 29.44±2.47 | F2断层泥 | 断层泥 | C2-5TL | 26.29±2.08 | F2断层泥 | 黏土 | C3-1TL | 14.99±1.20 | K48钻孔探槽顶部盖层 |
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