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Statements

Subject Item
dbr:Seismic_wide-angle_reflection_and_refraction
rdfs:label
Seismic wide-angle reflection and refraction
rdfs:comment
Seismic wide-angle reflection and refraction is a technique used in geophysical investigations of Earth's crust and upper mantle. It allows the development of a detailed model of seismic velocities beneath Earth's surface well beyond the reach of exploration boreholes. The velocities can then be used, often in combination with the interpretation of standard seismic reflection data and gravity data, to interpret the geology of the subsurface.
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dbc:Geophysics
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71383907
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1100424922
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dbr:Basalt dbr:Crust_(geology) dbr:S-wave dbr:Mantle_(geology) dbc:Geophysics dbr:Earthquake dbr:Seismometer dbr:Drilling_and_blasting dbr:P-wave dbr:Geophysics dbr:Ocean-bottom_seismometer dbr:Reflection_seismology dbr:Mantle_transition_zone dbr:Ray_tracing_(physics) dbr:Seismic_source dbr:Seismic_vibrator
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dbo:abstract
Seismic wide-angle reflection and refraction is a technique used in geophysical investigations of Earth's crust and upper mantle. It allows the development of a detailed model of seismic velocities beneath Earth's surface well beyond the reach of exploration boreholes. The velocities can then be used, often in combination with the interpretation of standard seismic reflection data and gravity data, to interpret the geology of the subsurface.
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wikipedia-en:Seismic_wide-angle_reflection_and_refraction