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- W2006984249 abstract "Historically, detection of anomalies using seismic methods has relied heavily on wavefield interference and point source radiation phenomena (Rechtien et al., 1995; Miller and Steeples, 1991; Steeples and Miller, 1988; Cook, 1965; Fisher 1971; Watkins et al., 1967). This approach can be effective in some situations, but considering the wealth of information contained in the wavefield, it is at best a cursory use of the information available in the wavefield. Recent development of surface seismic techniques designed to provide a quantitative measure of key seismic properties for each 3-D cell of a specified earth volume from a single shot gather by analyzing individual components of the wavefield has shown great promise (Miller et al., 2001). This project proved an incremental step in the evaluation of the potential of these seismic imaging and sampling techniques for shallow tunnel detection. Geologic or anthropogenic underground anomalies have been successfully identified using various components of the seismic wavefield and empirical correlations, some of these include: bedrock karst feature in southern Alabama and eastern Kansas (Miller and Xia, 1999; Miller et al., 1999), faulted and/or mined out zones in southern Illinois, buried pipes at Lawrenceville, Illinois (Miller et al., 2000) and San Jose, California, and a tunnel at 35 ft below ground surface at Otay Mesa, California (Miller et al., 2002)." @default.
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- W2006984249 date "2003-01-01" @default.
- W2006984249 modified "2023-09-26" @default.
- W2006984249 title "Seismic search for underground anomalies" @default.
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- W2006984249 doi "https://doi.org/10.1190/1.1817502" @default.
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