Wyoming Aeromagnetic Data
Processing
The assembly of 27 individual aeromagnetic surveys and grids
to create the Wyoming state-wide compilation was done in several
steps.
DATA PROCESSING STEPS
- Grids were constructed from the original aeromagnetic
survey data with a cell size of between 1/3 and 1/5 of
the flightline spacing of the survey, using a minimum
curvature gridding algorithm (Webring, 1982). For digitized contour line
data, the initial grid was constructed using a minimum
curvature algorithm and a spacing appropriate for the
scale of the digitized map.
- The Definitive Geomagnetic Reference Field (DGRF)
calculated (Sweeney, 1990) for the date of the original survey was
applied (in some cases this required the determination
and addition of the original reference field removed before removal of
the DGRF) .
- The original survey grids were continued to 304.8 meters (1000 feet)
above ground by converting to draped as
necessary. Upward continuation of the NURE and other draped surveys was by
standard 2D FFT filtering techniques. Level-to-drape
continuation was performed using the chessboard method
(Cordell and others,
1992).
- The survey grids were regridded, as necessary, to the
final grid cell size of 500 meters using a minimum curvature
algorithm.
- The datum levels of the converted grids were adjusted (by
addition or subtraction of a constant value) to minimize
differences at the boundaries.
- These adjusted grids were combined into a single merged
grid that shows the magnetic field measured or calculated
at 304.8 meters (1000 feet) above ground. This level was selected in order to be
compatible with adjacent state compilations in Utah (Bankey
and others, 1998), Montana (McCafferty, 1998),
and Colorado (Oshetski and Kucks, 2000).
ADDITIONAL PROCESSING STEPS OR INCONSISTENCIES
- Quadrangles of NURE surveys that consisted of 6 mile flight spacing (Cody,
Arminto, Casper, And Preston) were plugged using minimum curvature
interpolation to remove areas of no data within the Wyoming state boundary.
- Merging of NURE quadrangles at the 42oN latitude generated
lineations at the boundaries due to questionable compatibility of data sets.
- The border between Cody-Sheridan and Thermopolis-Arminto at the 44oN
latitude has a questionable merge boundary which may actually be
geologically controlled.
- The Sierra Madre (5040) survey has extensive flight-line noise problems
that are of unknown origin. The solution was to first remove any extremely
offending lines and then to micro-level the remaining lines. There still exists
some major shifts that appear to be in blocks of lines but they have been
allowed to remain.
- Miscellaneous herringbones exist within the map where the data quality was
beyond any reasonable recovery.
GRID PROJECTION SPECIFICATIONS
- Projection = Lambert conformal conic
- Central meridian = 107.5 degrees W
- Base latitude = 41 degrees N
- Standard parallels = 33 and 45 degrees N
- Semi-major ellipsoid axis = 6378206.4 m
- Eccentricity squared = 0.0067686579973
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