FIELD: physics.
SUBSTANCE: method is based on determining the vertical velocity of longitudinal elastic waves in an anisotropic medium from values of apparent reservoir and horizontal velocity, determined from reflection technique data with arrangement of signal sources and receivers on the surface. Vertical velocity (v0) in the selected layer is determined using the formula v0=0.53 Va+0.4 vh.
EFFECT: high accuracy of seismic probing data.
1 dwg
Authors
Dates
2013-09-10—Published
2011-11-17—Filed