DW TOMO

DW TOMO Refraction Tomography does not require layer assignment and phantom time-distance curves. The complex velocity structure can be directly estimated from first arrivals. This approach is especially suitable to derive the structure with no distinct layer interface due to the gradual velocity change where the traditional refraction interpretation methods are invalid.

DW TOMO utilizes the robust grid ray tracing and regularized inversion with constraints in tomography. The estimated velocity model can also be used for static correction in seismic reflection data processing.

Features

• Automatically or manually pick first arrivals with a trace magnifier
• Robust grid ray tracing
• Regularized iterative inversion with constraints
• Build an initial layered gradient model based on traveltime curvesnew
• Load a velocity file or interactively build an initial model
• Allow variable surface

• Check the picked and calculated first arrivals directly on seismic traces
• Fitting error analysis
• Interactively pause and resume or stop the tomography procedure
• Simultaneously update the display of first arrivals and ray paths
• Review the inverted model in each iteration
• Overlay velocity section with ray paths
• Plot well data on the velocity sectionnew
• Plot velocity section with colors, contours, and editable lithologic symbols

• Load all shots at one time
• Merge multiple TT curve files into one filenew
• Check and assign geometry with layout chart
• Input geometry as slope or horizontal distance for seismic data collected across
• topographynew
• Trigger delay correction
• Filter and scale seismic data with support of undo and redo functions