Gravity Anomaly Free Air Calculator

Land free-air anomaly in milligal: g_obs - g_ref + 0.3086 h with station elevation h in meters and the standard free-air gradient of 0.3086 milligal per meter.

Description

Land free-air anomaly in milligal: g_obs - g_ref + 0.3086 h with station elevation h in meters and the standard free-air gradient of 0.3086 milligal per meter.

Gravity Anomaly Free Air Calculator: Land free-air anomaly in milligal: g_obs - g_ref + 0.3086 h with station elevation h in meters and the standard free-air gradient of 0.3086 milligal per meter.

When to use Gravity Anomaly Free Air

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.

g obs
Observed absolute gravity at the station in milligal.
Elevation
Station elevation above the datum in meters.
g ref
Theoretical (normal) gravity at the station latitude and datum in milligal.

How Gravity Anomaly Free Air works

Land free-air anomaly in milligal: g_obs - g_ref + 0.3086 h with station elevation h in meters and the standard free-air gradient of 0.3086 milligal per meter. 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

Free-air anomaly
Free-air anomaly in milligal.
Free-air correction
Free-air correction 0.3086 h in milligal.

Limitations and assumptions

  • Classification diagrams and geochemical ratios require appropriate normalization, oxidation-state treatment, volatile basis, analytical quality, alteration screening, mineral or whole-rock context, and a composition within the method's calibration domain.
  • 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. Igneous petrology — Wikipedia contributors

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