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
Hauptverfasser: Hu, Ze-an, Zhang, Ping-song, Xu, Guang-quan
Format: Artikel
Sprache:eng
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