Relationship Between Geological Structures and Velocity Anomalies in Two-Dimensional Tomography with First-Arrival Seismic Travel Time (FAST): A New Recognization
Two-dimensional (2D) tomography with first-arrival seismic travel time (FAST) is widely and effectively used to detect geological anomalies. For detecting small geostructures in a coalbed, 2D seismic tomography with FAST depends primarily on the seismic wave velocity. The seismic velocity tomography...
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Veröffentlicht in: | Geotechnical and geological engineering 2019-04, Vol.37 (2), p.561-569 |
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