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The application of seismic exploration method to ctive faults detection in urban thin overburden area |
Dong-Wei MA |
Shengfeng Institute of Geological New Technique Application of Shanghai,Shanghai 201702,China |
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Abstract Currently,seismic explorations is the main geophysical prospecting method for detecting active fault lines in cities.In the detection of the active faults in Xinyi City,the wave reflected from the top of bed rock can only be recognized using P-wave reflection due to the thin overburden in local area.In general,it is difficult to determine the exact location of a fault and the burial depth of the upper breaking point based on the change of a single coaxial axis in seismic reflection profile.The method of S-wave reflection is characterized by high resolution and strong stratification capability,which can make up for the shortcomings of P-wave reflection exploration,thus improving the precision of exploration.In addition,there exist strata of two different ages on both sides of some faults in this exploration area,and there are obvious differences in velocity between them.The seismic velocity profile obtained by seismic tomography can reflect the changes of underground velocity structures and also reveal the existence of shallow faults.Through this comparison and comprehensive analysis of the results obtained by these geophysical prospecting methods and the combination of geological data,the ideal geophysical prospecting results and sound exploration results are reached.
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Received: 31 January 2019
Published: 25 October 2019
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Map showing faults and seismic profiles in Xinyi city
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参数 | L1测线纵波 | L1测线横波 | L2测线纵波 | 采样间隔/ms | 0.5 | 0.5 | 0.5 | 记录长度/ms | 1 024 | 1 024 | 1 024 | 接收道数/道 | 72 | 96 | 120 | 道间距/m | 2 | 2 | 3 | 炮距/m | 6 | 6 | 9 | 覆盖次数/次 | 12 | 16 | 20 | 激发方式 | 单边(最小偏移8 m) | 端点 | 中间对称 | 震源出力/% | 70 | 40 | 70 | 扫频范围/Hz | 10~120 | 10~100 | 10~120 | 扫描时长/s | 10 | 10 | 10 |
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List of construction parameters of reflection method
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Single shot comparison chart of P(a) and S(b) wave across the fault of L1 line
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Diagram of seismic refraction tomographic method observation system
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A typical refraction seismic record section
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P-wave time section of L1 line
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S-wave time section of L1 line
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P-wave time section of L2 line
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Refraction tomography profile of L2 line
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