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
-
Igneous petrology — Wikipedia contributors
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