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OF 2008-1089: Data Processing Details

Airborne Gravity Survey and Ground Gravity in Afghanistan: A Website for Distribution of Data

Afghanistan Airborne Bouguer Gravity Anomaly Map at 7,000 m Above Ground

Afghanistan Airborne Bouguer Gravity Anomaly Map at 7000 m Above Ground

AIRBORNE FLIGHT AND DATA PROCESSING DETAILS

1. Gravity measurements were made by two ZLS Corporation-upgraded LaCoste and Romberg S gravimeters mounted in the center of the fuselage.

2. Aircraft positioning was determined from GPS measurements in the aircraft and at base stations at Kandahar, Herat, Shebergan, and Kabul using differential interferometric techniques. The GPS-derived positions were coupled with the output of an inertial measurement unit to provide aircraft attitude information.

3. The airborne gravimeter data were corrected for aircraft vertical acceleration, free-air and Eötvös effects, normal gravity, and platform off-level effects.

4. High-frequency noise was attenuated using a low-pass filter resulting in along-track resolution of approximately 20-25 km (half-wavelength) at survey speeds of 300-370 kts. The noise was further reduced by averaging data from the two gravimeters.

5. A least-squares network adjustment was applied to the survey to minimize intersection differences (Peters and Brozena, 1988).

6. The FAA values supplied by NRL were draped at a constant level of 7 kilometers above the ground using the 1D Compudrape function in the Oasis montaj software. This was accomplished using 50 continuation levels and a high-cut factor of 2.

7. The combined Bouguer slab and terrain corrections, or the effect of all mass above sea level assuming a density of 2.67 g/cc, were computed using the algorithm of Parker (1972) within GM-SYS 3D software.

8. The Bouguer and terrain corrections were low-pass filtered using an 8th order 1D Butterworth filter in order to simulate the frequency content of the FAA profiles. A filter cutoff of 40 kilometers was found to be appropriate for the entire dataset.

9. Each survey segment, defined on the basis of flight line direction, was gridded using minimum curvature in order to create a series of complete Bouguer anomaly grids.

10. Residual flight-line noise from each complete Bouguer anomaly grid was removed using decorrugation.

11. The grids were merged together using only static shifts between grids.

12. Remaining high-frequency noise resulting from the above processing steps was removed using a low-pass 8th order Butterworth filter with a cutoff of 15 kilometers.



Afghanistan Ground Bouguer Gravity Anomaly Map Continued to 7,000 m Above Ground

Afghanistan Ground Gravity Anomaly Map Continued to 7,000 m Above Ground

GROUND GRAVITY SURVEY

Ground gravity station data were collected by members of the Afghanistan Water and Soil Survey Authority during 1966 and 1967 (McGinnis, 1971).

COMPOSITE (AIRBORNE AND GROUND) GRAVITY GRID

The image displayed on the title page of the report was generated by using Geosoft Oasis 'grid mosaic' function to composite the airborne and ground gravity grids into a final grid that depicts the complete Bouguer anomaly (CBA) field at 7,000 m above ground.


Afghanistan Isostatic Gravity Anomaly Map at 7,000 m Above Ground

Afghanistan Isostatic Gravity Anomaly Map of Composite CBA

ISOSTATIC GRAVITY ANOMALY GRID OF PREVIOUS COMPOSITE GRID

The isostatic gravity anomaly was created from the CBA grid using the Geosoft Oasis program, which uses the method of Simpson and others (1986), and the following parameters: Depth of compensation =30 km, density=2.67 and Moho contrast density=.33 g/cc.

PROJECTION SPECIFICATIONS

All databases, maps, grids, and xyz files in this report use the following projection specifications:

  • Projection = Transverse Mercator
  • Central meridian = 66 degrees E
  • Base latitude = 34 degrees N
  • Scale factor = 0.9996
  • Semi-major ellipsoid axis = 6378137 m
  • Eccentricity = 0.08181919084
  • Horizontal datum = WGS 84
  • Ellipsoid = WGS 84

REFERENCES

  • McGinnis, L.D., 1971, Gravity fields and tectonics in the Hindu Kush: Journal of Geophysical Research, v. 76, no. 8, p. 1894-1904.
  • Parker, R.L., 1972, The rapid calculation of potential anomalies: Geophysical Journal of the Royal Astronomical Society, v. 31, p. 447-455.
  • Peters, M.F., and Brozena, J.M., 1988, Constraint criteria for adjustment of potential field surveys: Geophysics, v. 53, no. 12, p. 1601-1604.
  • Simpson, R.W., Jachens, R.C., Blakely, R.J., and Saltus, R.W., 1986, A new isostatic residual gravity map of the conterminous United States with a discussion of the significance of isostatic residual anomalies: Journal of Geophysical Research, v. 91, p. 8348-8372.
  • U.S. Geological Survey, 2006, Aeromagnetic and gravity surveys in Afghanistan: A Website for Distribution of Data: U.S. Geological Survey Open-File Report 2006-1204, available at URL https://pubs.usgs.gov/of/2006/1204/

DATA PRODUCTS

All grids are presented in Geosoft binary grid format, with two files describing each of the grids (suffixes .grd and .gi). All databases are presented in two formats: Geosoft binary database format and Geosoft ASCII XYZ format. All formats can be converted using the free conversion software offered by Geosoft at http://www.geosoft.com/.

  1. Afghan_airborne_gravity.gdb - Database of airborne gravity data.
  2. Afghan_ground_gravity.gdb - Database of ground gravity data.
  3. Afghan_airborne_gravity.XYZ - ASCII XYZ file of airborne gravity data (output of .gdb file above).
  4. Afghan_ground_gravity.XYZ - ASCII XYZ file of ground gravity data (output of .gdb file above).
  5. Afghan_airborne_gravity_cba.grd - Grid of airborne complete Bouguer gravity data at 1,000 m grid spacing at 7,000 m above terrain.
  6. Afghan_ground_gravity_cba.grd - Grid of ground complete Bouguer gravity data from the U.S. Geological Survey (USGS, 2006) at 2,000 m grid spacing at 7,000 m above terrain.
  7. Afghan_total_gravity_cba.grd - Grid of composite (airborne and ground) complete Bouguer gravity grids at 1,000 m grid spacing at 7,000 m above terrain.
  8. Afghan_total_gravity_iso.grd - Grid of isostatic gravity anomaly calculated from the previous composite (airborne and ground) complete Bouguer gravity grid. Parameters used in the calculation are density of topo load=2.67 g/cc, depth of root at sea level=30 km, and density contrast at depth=.33 g/cc
  9. Afghan_iso.pdf - Map of the isostatic residual gravity anomaly of Afghanistan.
  10. README_gravity_database_description.doc - Description of data products.

DATA ACCESS

This web site makes available to users the data products for the surveys listed above:

To view the DATA directory, click on DATA.

To access the README file ("README_gravity_database_description.txt") describing the gravity data product files, click on README.

Version 1.0

Posted April 2008

For more information about this
report contact: Jared Abraham

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