summary-data-locations: Identification numbers, coordinates, sample descriptions, and summary ages of each sample step-heating-data: Power output levels and resultant measurements from each sample run
Benowitz, J.A., Layer, P.W., Freeman, L.K., Griesel, G.A., Elliott, B.A., Szumigala, D.J., Wypych, Alicja, and Montayne, Simone, 2018, 40Ar/39Ar data from the eastern Moran area, Tanana B-6 and C-6 quadrangles, and the Ruby mining district, Ruby B-5 and B-6 quadrangles, Alaska: Raw Data File RDF 2018-5, Alaska Division of Geological & Geophysical Surveys, Fairbanks, Alaska, United States.Online Links:
This is a point data set.
Horizontal positions are specified in geographic coordinates, that is, latitude and longitude. Latitudes are given to the nearest 0.000001. Longitudes are given to the nearest 0.000001. Latitude and longitude values are specified in decimal degrees.
The horizontal datum used is North American Datum of 1927.
The ellipsoid used is Clarke 1866.
The semi-major axis of the ellipsoid used is 6378206.40000000037.
The flattening of the ellipsoid used is 1/294.978698199999997.
Generic example of a sample identifier: YYAAA9999X: YY=last two digits of the year the sample was collected, AAA=geologist's initials (one to three characters), 9999=unique station number, X= optional alpha character which indicates that multiple samples were collected at a given location or that multiple observations were recorded in the project database.
The lab sample number is typically identical to the field sample number. However, in some cases, the sample number provided by the lab does differ from the number assigned in the field. We provide both numbers to document instances in which the sample numbers in the lab files differ from the field sample number.
The samples presented in this report were collected by the authors or other DGGS staff.
Range of values | |
---|---|
Minimum: | -155.790105 |
Maximum: | -152.604273 |
Units: | decimal degrees |
Range of values | |
---|---|
Minimum: | 64.463951 |
Maximum: | 65.467821 |
Units: | decimal degrees |
The type of material that was selected for dating varied according to mineral composition and grainsize of the submitted rock sample. This field specifies whether the age was derived from a mineral separate (generally 1 to 10 individual crystals dated together as a single run), a single crystal, or the whole rock.
The minerals selected for dating would typically be grains of biotite, hornblende, or muscovite.
A brief sample or station description.
Map unit designations are based on geologic mapping and petrographic observations.
Map unit designations are based on concurrent geologic mapping or previously published reports. A comprehensive reference list is provided in the accompanying report.
The values are a concatenation of the integrated age determination and the calculated error associated with the integrated age determination
Value | Definition |
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NULL | A NULL or blank values indicates that the PLATEAU_AGE_MA value was not calculated by the lab |
The values are a concatenation of the plateau age determination and the calculated error associated with the plateau age determination
Range of values | |
---|---|
Minimum: | 49.1 |
Maximum: | 99.3 |
Units: | percent |
Value | Definition |
---|---|
NULL | A NULL or blank values indicates that the value was not calculated by the lab |
Value | Definition |
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NULL | A NULL or blank values indicates that the PLATEAU_REMARKS value was not provided by the lab |
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Value | Definition |
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NULL | A NULL or blank values indicates that the W_M_AGE_MA value was not calculated by the lab |
The values are a concatenation of the weighted average age determination and the calculated error associated with the weighted mean average age determination
Range of values | |
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Minimum: | 56.6 |
Maximum: | 56.6 |
Units: | percent |
Value | Definition |
---|---|
NULL | A NULL or blank values indicates that the value was not calculated by the lab |
Value | Definition |
---|---|
NULL | A NULL or blank values indicates that the W_M_AGE_REMARKS value was not provided by the lab |
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Value | Definition |
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NULL | A NULL or blank values indicates that the ISOCHRON_AGE value was not provided by the lab |
The values are a concatenation of the isochron age determination and the calculated error associated with the isochron age determination
Value | Definition |
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NULL | A NULL or blank values indicates that the value was not calculated by the lab |
Range of values | |
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Minimum: | 0.13 |
Maximum: | 1.59 |
Value | Definition |
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NULL | A NULL or blank values indicates that the ISOCHRON_REMARKS value was not provided by the lab |
Free text
A discussion of the preferred age for each analysis is provided in the accompanying lab report. The possible values are: plateau, isochron, weighted average, or integrated.
The preferred age for each analysis is discussed in detail in the accompanying lab report.
Generic example of a sample identifier: YYAAA9999X: YY=last two digits of year, AAA=geologist's initials (one to three characters), 9999=unique station number, X= optional alpha character which indicates that multiple samples were collected at a given location or that multiple observations were recorded in the project database.
The lab sample number is typically identical to the field sample number. However, in some cases, the sample number provided by the lab does differ from the number assigned in the field. We provide both numbers to document instances in which the sample numbers in the lab files differ from the field sample number.
Value | Definition |
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NULL | A NULL or blank values indicates that the values in the row were calculated by weighting the individual heating steps by the fraction of 39Ar released. |
Range of values | |
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Minimum: | 300 |
Maximum: | 9000 |
Units: | megawatts |
Value | Definition |
---|---|
NULL | The values in the row were derived from a heating step |
Integrated | the values in this row were calculated by weighting the individual heating steps by the fraction of 39Ar released |
Value | Definition |
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NULL | A NULL or blank values indicates that the value was not applicable or not calculated by the lab |
Range of values | |
---|---|
Minimum: | 0.0011 |
Maximum: | 1 |
Range of values | |
---|---|
Minimum: | 9.59019 |
Maximum: | 2155.92823 |
Range of values | |
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Minimum: | 0.05292 |
Maximum: | 142.8695 |
Range of values | |
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Minimum: | -0.22738 |
Maximum: | 38.19865 |
Range of values | |
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Minimum: | 0.00006 |
Maximum: | 1.31526 |
Range of values | |
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Minimum: | -0.01753 |
Maximum: | 7.05618 |
Range of values | |
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Minimum: | 0.00003 |
Maximum: | 0.46725 |
Range of values | |
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Minimum: | -28.45257 |
Maximum: | 98.48928 |
Range of values | |
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Minimum: | 0.03976 |
Maximum: | 51.8597 |
Range of values | |
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Minimum: | -0.41715 |
Maximum: | 72.03245 |
Range of values | |
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Minimum: | 0.00011 |
Maximum: | 2.47635 |
Range of values | |
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Minimum: | -0.00458 |
Maximum: | 0.23006 |
Range of values | |
---|---|
Minimum: | 0.00001 |
Maximum: | 0.01315 |
Range of values | |
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Minimum: | 2.85421 |
Maximum: | 73.04206 |
Range of values | |
---|---|
Minimum: | 0.04818 |
Maximum: | 38.81533 |
Range of values | |
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Minimum: | 20.47 |
Maximum: | 462.13 |
Units: | MA |
Range of values | |
---|---|
Minimum: | 0.55 |
Maximum: | 246.42 |
Units: | MA |
WeightedAverageOfJFromStandards value and error
This study is part of the Alaska Airborne Geophysical/Geological Mineral Inventory Program funded by the Alaska State Legislature. The research was also supported by the U.S Geological Survey, National Cooperative Geologic Mapping Program, under STATEMAP award number G11AC20203. Access to Doyon Limited lands and to drill core from the Monday Creek prospect stored in Fairbanks, as well as permission to collect samples and publish data was kindly granted by Doyon Limited.
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This work was part of an integrated geological, geophysical, and geochemical mineral inventory study in the eastern Kokrines Hills near Moran Dome in the Tanana B-6 and C-6 quadrangles. Previous geologic work in the area is at a reconnaissance scale, although two localities in the study area have undergone detailed mineral-resource evaluations (Tozimoran Creek Placer and Monday Creek). No geochronological data from the area have been published, but limited geochronology has been published from the region.
Freeman, L.K., Szumigala, D.J., Blessington, M.J., and Werdon, M.B., 2012, Geochemical trace-element and rare-earth element data from stream-sediment and pan-concentrate samples collected in 2011 in the Melozitna mining district, Tanana and Melozitna quadrangles, interior Alaska: Raw Data File RDF 2012-3, Alaska Division of Geological & Geophysical Surveys, Fairbanks, Alaska, United States.Online Links:
Lough, T.A., Freeman, L.K., Elliott, B.A., Griesel, G.A., Newberry, R.J., and Szumigala, D.J., 2012, Geochemical, major-oxide, minor-oxide, trace-element, and carbon data from rocks collected in 2011 in the Moran area, Tanana and Melozitna quadrangles, Alaska: Raw Data File RDF 2011-4 v. 2, Alaska Division of Geological & Geophysical Surveys, Fairbanks, Alaska, United States.Online Links:
This data set is being released into the DGGS Raw Data File series. The information has been examined by several geologists familiar with the study area, but the data and accompanying report have not been formally reviewed for technical content or for conformity to the editorial standards of DGGS. Questions regarding the accuracy of the analytical values can be best answered by the originating lab.
Location data for samples collected during the 2011 DGGS field campaign were derived using Garmin eTrex hand-held GPS units. Waypoints were downloaded from the eTrex units and merged with a hand-transcribed Microsoft Access field notes database on a daily basis, and locations were spot checked to ensure that the data merge was correct. Location error for this process is estimated to range between 3 and 20 m. The North American Datum of 1927 (NAD27) was used consistently for recording and reporting sample locations. Sample 11LF004A used the coordinates for the drill hole collar, which were transformed into NAD27 from World Geodetic System of 1984 coordinates provided by Doyon, Limited. The error for this sample is less than 10 m. Samples from the Ruby mining district were digitized from sample locations depicted on georeferenced images of scanned geologic map sheets (Puchner and others, 1998); these samples were collected prior to the use of GPS, and locations were hand plotted by geologists on USGS 1:63,360 topographic maps. Cumulative error for these locations could be in excess of 100 m. Sample RM 23241-R was collected from sluice box concentrates and the source is at or below the confluence of Ash and Tozimoran creeks. The location provided is for the creek confluence, and a location error of 1,000 m is assigned to this sample.
This data release is complete.
not applicable
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- Access_Constraints:
- This report, map, and/or dataset is available directly from the State of Alaska, Department of Natural Resources, Division of Geological & Geophysical Surveys (see contact information below).
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RDF 2018-5
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DGGS publications are available as free online downloads or you may purchase paper hard-copies or digital files on CD/DVD or other digital storage media by mail, phone, fax, or email from the DGGS Fairbanks office. To purchase this or other printed reports and maps, contact DGGS by phone (907-451-5020), e-mail (dggspubs@alaska.gov), or fax (907-451-5050). Payment accepted: Cash, check, money order, VISA, or MasterCard. Turnaround time is 1-2 weeks unless special arrangements are made and an express fee is paid. Shipping charge will be the actual cost of postage and will be added to the total amount due. Contact us for the exact shipping amount.
Data format: | ASCII tabular files |
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Network links: |
<http://doi.org/10.14509/30117> |
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