Entity_and_Attribute_Overview:
Airborne survey specifications
These items are constant for the entire survey
Project number: 6005
Project name: Southeast Arizona
Survey flown by: Texas Instruments, Inc.
Survey flown for: DOE Grand Junction Office
Approx. no. of line miles: 8607
Survey height: 400 ft
Altitude method: Draped over terrain
Flight-line spacing: 3 miles
Flight-line direction: North-South
Aircraft used: Douglas DC-3
Airport - arrival: unknown
Airport - departure: unknown
Magnetometer used: Geometrics G-803
Sensor tow distance: 100 feet
Radiometric crystal package volume: 2493 (down) & 415 (up) cu. in.
Entity_and_Attribute_Detail_Citation:
Nettleton, L.L., 1971, Elementary Gravity and Magnetics for
Geologists and Seismologists: Society of Exploration Geophysicists
Monograph Series No. 1, p. 83-87.
Dobrin, M.B., 1976, Introduction to Geophysical
Prospecting: New York, McGraw-Hill Book Company,
p. 505-517.
Grasty, R.L., and Holman, P.B., 1974, Optimum Detector Sizes for
Airborne Gamma-ray Surveys: Geological Survey of Canada Paper
74-1, Part B, p. 72-74.
Entity_and_Attribute_Overview:
Aeromagnetics
Each record contains the following 12 attributes:
No name contents
1 line flight line number
2 fid fiducial number (integer)
3 time time (hhmmss)
4 day Julian day flown (integer)
5 year year flown (integer)
6 latitude latitude (decimal degrees)
7 longitude longitude (decimal degrees)
8 radalt radar altimeter reading above ground (meters)
9 totmag corrected magnetic value (nT)
10 resmag residual magnetic value (nT)
11 diurnal ground magnetometer value (nT)
12 geology surficial geology beneath flight line (coded)
Entity_and_Attribute_Detail_Citation:
Nettleton, L.L., 1971, Elementary Gravity and Magnetics for
Geologists and Seismologists: Society of Exploration Geophysicists
Monograph Series No. 1, p. 83-87.
Dobrin, M.B., 1976, Introduction to Geophysical
Prospecting: New York, McGraw-Hill Book Company,
p. 505-517.
Entity_Type:
Entity_Type_Label: record for one magnetic or radiometric data point
Entity_Type_Definition:
The set of all measurements reported for a magnetic or radiometric
data point having the same spatial location.
Entity_Type_Definition_Source:
Standard aeromagnetic and aeroradiometric data collection procedures
as written in the contract for survey collection.
Attribute:
Attribute_Label: line
Attribute_Definition: flight line number
Attribute_Definition_Source: often assigned by airborne survey crew
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 1
Range_Domain_Maximum: 106
Attribute_Units_of_Measure: alphanumeric value
Attribute:
Attribute_Label: fid
Attribute_Definition:
A fiducial number is a mark which indicates points of
simultaneity. It is a user-defined integer used during
airborne operations to correlate recording devices (magnetometers)
with navigational records (altimeters, camera film, strip charts)
that were recorded at the same time.
Attribute_Definition_Source:
Sheriff, R.E., 1984, Encyclopedic dictionary of
exploration geophysics: Tulsa, OK, Society of
Exploration Geophysicists, p. 89.
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 0
Range_Domain_Maximum: 88723
Attribute:
Attribute_Label: time
Attribute_Definition:
time of data point collection. Time is given
in either local time or Greenwich Meridian Time.
Values of 9999 indicate missing data.
Attribute_Definition_Source: self evident
Attribute_Domain_Values:
Unrepresentable_Domain:
a range of time of day values has no meaning
because the timeframe can span several days or weeks.
Attribute:
Attribute_Label: day
Attribute_Definition:
Julian day, where Jan. 1 = 1 and
Dec. 31 = 365 or 366 (leap year)
Attribute_Definition_Source: self evident
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 11
Range_Domain_Maximum: 346
Attribute_Value_Accuracy_Information:
Attribute_Value_Accuracy: 1
Attribute_Value_Accuracy_Explanation: Both beginning and end Julian dates were taken from dataset.
Attribute:
Attribute_Label: year
Attribute_Definition: year of data point collection
Attribute_Definition_Source: self evident
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 1974
Range_Domain_Maximum: 1975
Attribute:
Attribute_Label: latitude
Attribute_Definition: latitude - geographic coordinate
Attribute_Definition_Source: self evident
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 31.3333
Range_Domain_Maximum: 33.5574
Attribute_Units_of_Measure: decimal degrees
Attribute:
Attribute_Label: longitude
Attribute_Definition: longitude - geographic coordinate
Attribute_Definition_Source: self evident
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: -111.7227
Range_Domain_Maximum: -109.0333
Attribute_Units_of_Measure: decimal degrees
Attribute:
Attribute_Label: radaralt
Attribute_Definition:
radar altimetry reading, in meters
An aircraft navigational system in which short electromagnetic waves
are transmitted, and the energy scattered back by reflection
is detected. From this measurement, the distance between the aircraft
and the ground is calculated and recorded as radar altimetry.
Values of -999.9 indicate missing data.
Attribute_Definition_Source:
Sheriff, R.E., 1984, Encyclopedic dictionary of exploration geophysics:
Tulsa, OK, Society of Exploration Geophysicists, p. 89.
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 45.1
Range_Domain_Maximum: 1047.9
Attribute_Units_of_Measure: meters
Attribute:
Attribute_Label: totmag
Attribute_Definition:
Raw magnetic value with base magnetometer corrections applied.
Because the magnetic field of the earth varies diurnally,
a stationary base magnetometer is maintained on the ground
during airborne surveying. The base magnetometer records
changes in the magnetic field (in nanoTeslas) as a function
of time. The magnetic changes may have an amplitude of 20
to 50 nanoTeslas. If changes are more severe, as would
occur from a magnetic storm, surveying is discontinued or
the data recorded are not used.
Diurnal variations are then removed from the airborne magnetic
data based on the common time.
Records containing missing data were usually deleted.
Attribute_Definition_Source:
see: Nettleton, L.L., 1971, Elementary Gravity and Magnetics for
Geologists and Seismologists: Society of Exploration Geophysicists
Monograph Series No. 1, p. 83-87.
A description of magnetometers and how they measure
the total magnetic field can be found in:
Dobrin, M.B., 1976, Introduction to Geophysical
Prospecting: New York, McGraw-Hill Book Company,
p. 505-517.
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: 48035.0
Range_Domain_Maximum: 57224.0
Attribute_Units_of_Measure: nanoTeslas
Attribute_Value_Accuracy_Information:
Attribute_Value_Accuracy: 2
Attribute_Value_Accuracy_Explanation:
The airborne magnetometer is accurate to about 1 nanoTesla,
and the base magnetometer has the same accuracy. The accuracy
of the base-corrected airborne value therefore is near 2 nanoTeslas
or better.
Attribute_Measurement_Frequency:
The magnetometer has a recharging interval of 0.5
seconds. The data were recorded at 2 second intervals.
Attribute:
Attribute_Label: resmag
Attribute_Definition:
residual magnetic value
The total magnetic value minus a geomagnetic reference field (GRF),
which is a long-wavelength regional magnetic field. The most commonly
used reference field is determined from a model developed by the
International Association of Geomagnetism and Aeronomy (IAGA). The
International Geomagnetic Reference Field (IGRF), is a predictive model
adopted at the beginning of a model period (e.g. in 1989 for 1990-1995).
After the model period, a revised definitive model is adopted, the DGRF.
This is the preferred model to use for removing regional magnetic fields.
For this survey, the field removed is IGRF 1965.
Some contractors add a constant to the residual value in order to
avoid negative values. This constant can vary from one data set to
another.
Values of -9999.9 indicate missing data.
Attribute_Definition_Source:
Nettleton, L.L., 1971, Elementary Gravity and Magnetics for
Geologists and Seismologists: Society of Exploration Geophysicists
Monograph Series No. 1, p. 83-87.
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: -9999.9
Range_Domain_Maximum: -9999.9
Attribute_Units_of_Measure: nanoTeslas
Attribute_Value_Accuracy_Information:
Attribute_Value_Accuracy: 2
Attribute_Value_Accuracy_Explanation:
The Geomagnetic Reference Field that was subtracted from
the total magnetic value is based on a model, which was
updated to the date of the survey. New models are
available at five year intervals. These models have
vayring degrees of accuracy in determining the local
reference field.
Attribute:
Attribute_Label: diurnal
Attribute_Definition:
Base magnetometer values used to correct the total magnetic
value.
Because the magnetic field of the earth varies diurnally,
a stationary base magnetometer is maintained on the ground
during airborne surveying. The base magnetometer records
changes in the magnetic field (in nanoTeslas) as a function
of time called the diurnal. The magnetic changes may have an
amplitude of 20 to 50 nanoTeslas. The diurnal is monitored
during the survey and if changes are severe, as would
occur from a magnetic storm, surveying is discontinued or
the data recorded are not used.
Diurnal variations are then removed from the airborne magnetic
data based on the common time.
Values of -9999.9 indicate missing data.
Attribute_Definition_Source:
see: Nettleton, L.L., 1971, Elementary Gravity and Magnetics for
Geologists and Seismologists: Society of Exploration Geophysicists
Monograph Series No. 1, p. 83-87.
A description of magnetometers and how they measure
the total magnetic field can be found in:
Dobrin, M.B., 1976, Introduction to Geophysical
Prospecting: New York, McGraw-Hill Book Company,
p. 505-517.
Attribute_Domain_Values:
Range_Domain:
Range_Domain_Minimum: -9999.9
Range_Domain_Maximum: -9999.9
Attribute_Units_of_Measure: nanoTeslas
Attribute_Value_Accuracy_Information:
Attribute_Value_Accuracy: 2
Attribute_Value_Accuracy_Explanation:
The airborne magnetometer is accurate to about 1 nanoTesla,
and the base magnetometer has the same accuracy. The accuracy
of the base-corrected airborne value therefore is near 2 nanoTeslas
or better.
Attribute_Measurement_Frequency:
The base magnetometer has a recharging interval of 0.5
seconds. The data were recorded at 2-4 second intervals.
Attribute:
Attribute_Label: geology
Attribute_Definition:
Geologic identification codes or numeric codes indicating the rock
types immediately beneath the flight line. These codes were determined by
plotting the flight lines on a surficial geologic map. A description
of the codes can be found in the GJBX- or GJO- report for this
quadrangle listed in the Cross Reference section above.
Values of -99 indicate missing data.
Attribute_Definition_Source: original publication
Attribute_Domain_Values:
Unrepresentable_Domain: values are not quantified