Three-dimensional density variable-velocity seismic reflection spatial correction method
A seismic reflection, three-dimensional technology, applied in the field of geophysical exploration, to achieve the effect of improving accuracy, improving seismic velocity, and solving practical geological problems
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[0042] The original three-dimensional residual density body used in the present invention includes coordinate X, coordinate Y, coordinate Z, residual density Δσ (such as figure 1 ) and seismic velocity data body, including coordinate X, coordinate Y, reflection layer name LName, reflection layer time T, reflection layer velocity V, average velocity Va, reflection layer interface buried depth H and other data.
[0043] 1) Use seismic velocity data body: coordinate X, coordinate Y, reflection layer name LName, and each reflection layer time T, reflection layer velocity V, average velocity Va, reflection layer interface buried depth H and other data, and calculate each reflection layer The thickness D.
[0044] 2) Use the gravity three-dimensional residual density volume data: coordinate X, coordinate Y, coordinate Z, three-dimensional residual density Δσ, and calculate the bottom boundary depth GD and thickness GThick of the gravity three-dimensional residual density data.
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