Seismic Migration Aperture Calculator

Horizontal migration aperture for a dipping reflector: z tan(dip) per side (and twice that for the full aperture), with reflector depth z in meters and dip angle in degrees.

Description

Horizontal migration aperture for a dipping reflector: z tan(dip) per side (and twice that for the full aperture), with reflector depth z in meters and dip angle in degrees.

Seismic Migration Aperture Calculator: Horizontal migration aperture for a dipping reflector: z tan(dip) per side (and twice that for the full aperture), with reflector depth z in meters and dip angle in degrees.

When to use Seismic Migration Aperture

Use this geological calculation for a transparent first-pass interpretation of measured rock, soil, fluid, well, stratigraphic, isotopic, geophysical, or seismic data under an explicitly selected model.

z
Reflector depth in meters.
dip
Reflector dip angle in degrees.

How Seismic Migration Aperture works

Horizontal migration aperture for a dipping reflector: z tan(dip) per side (and twice that for the full aperture), with reflector depth z in meters and dip angle in degrees. The tool evaluates the supplied inputs together and returns the named outputs below; it does not infer omitted operating conditions or change the units shown.1

Aperture
One-sided horizontal migration aperture in meters.
Full aperture
Full horizontal migration aperture in meters.

Limitations and assumptions

  • Seismic magnitudes, moments, travel times, velocities, resolution, and energy depend on instrument correction, Earth model, phase picking, geometry, attenuation, radiation pattern, bandwidth, and calibration range. Magnitude scales are not universally interchangeable.
  • Use finite inputs in the displayed units and preserve more precision than the final presentation requires. Independently verify safety-critical, financial, compliance, or production decisions.

Alternative or Complementary approaches

Compare independent measurements and models, retain units and analytical metadata, propagate uncertainty, and validate interpretations against logs, cores, maps, laboratory data, or field observations.

References

  1. Seismology — Wikipedia contributors

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