u-pb zircon geochronology results from the provo and ...11. common pb correction is from measured...
TRANSCRIPT
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U-Pb Zircon Geochronology Results from the Provo and Duchesne 30' x 60'
Quadrangles, Utah
OPEN-FILE REPORT 719 UTAH GEOLOGICAL SURVEY
a division of UTAH DEPARTMENT OF NATURAL RESOURCES
2020
by
Utah Geological Survey, Kurt N. Constenius1, and Arizona LaserChron Center
1 UGS Contract Mapper, now Department of Geosciences, University of Arizona, Tucson
Suggested citation:
Utah Geological Survey, Constenius, K.N., and Arizona LaserChron Center, 2020, U-Pb zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah: Utah Geological Survey Open-File Report 719, variously paginated, https://doi.org/10.34191/OFR-719.
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Blank pages are intentional for printing purposes.
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INTRODUCTION
This Open-File Report makes available raw analytical data from laboratory procedures completed to determine the age of rock samples collected during geologic investigations funded or partially supported by the Utah Geological Survey (UGS) and the U.S. Geological Survey National Cooperative Geologic Mapping Program (STATEMAP). The references listed in table 1 gener-ally provide additional information such as sample location, geologic setting, and significance or interpretation of the samples in the context of the area where they were collected. The data were collected in the lab by K.N. Constenius and prepared by the Arizona Laserchron Center, Department of Geosciences, University of Arizona, Tucson, Arizona, under contract to the UGS. These data are highly technical in nature and proper interpretation requires considerable training in the applicable geochrono-logic techniques.
The data can be accessed electronically as an attachment to the PDF file of this report and are available at https://ugspub.nr.utah.gov/publications/open_file_reports/ofr-719/ofr-719.zip.
DISCLAIMER
This open-file release is intended as a data repository for information gathered in support of various UGS projects. The data are presented as received from Arizona LaserChron Center and do not necessarily conform to UGS technical, editorial, or policy standards; this should be considered by an individual or group planning to take action based on the contents of this report. The Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding the suitability of this product for a particular use. The Utah Department of Natural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users of this product.
The views and conclusions contained in this document are those of the authors and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the U.S. Government.
ACKNOWLEDGMENTS
Geologic mapping of the Provo and Duchesne 30' x 60' quadrangles was funded by the UGS and U.S. Geological Survey, National Cooperative Geologic Mapping Program (NCGMP). Provo was funded through USGS STATEMAP award num-bers 99HQAG0138 (1999-2000), 01HQAG100 (2001-02), 02HQAG055 (2002-03), 03HQAG0096 (2003-04), 04HQAG0040 (2004-05), 05HQAG0084 (2005-06), and 06HQAG0037 (2006-07). Duchesne was funded through USGS STATEMAP award numbers G12AC20226 (2012-13), G13AC00169 (2013-14), G14AC00214 (2014-15), G15AC00249 (2015-16), and G16AC00191 (2016-17).
REFERENCES
Constenius, K.N., Clark, D.L., King, J.K., and Ehler, J.B., 2011, Interim geologic map of the Provo 30' x 60' quadrangle, Utah, Wasatch, and Salt Lake Counties, Utah: Utah Geological Survey Open-File Report 586DM, 42 p., 2 plates, scale 1:62,500, contains GIS data, DVD, https://doi.org/10.34191/OFR-586DM.
Constenius, K.N., Coogan, J.K., Clark, D.L., and King, J.K., in preparation, Geologic map of the Provo 30' x 60' quadrangle, Utah, Wasatch, and Salt Lake Counties, Utah: Utah Geological Survey Map, scale 1:62,500.
Sprinkel, D.A., 2018, Interim geologic map of the Duchesne 30' x 60' quadrangle, Duchesne and Wasatch Counties, Utah: Utah Geological Survey Open-File Report 689, 37 p., 2 plates, scale 1:62,500, https://doi.org/10.34191/OFR-689.
Sprinkel, D.A., in preparation, Geologic map of the Duchesne 30' x 60' quadrangle, Duchesne and Wasatch Counties, Utah: Utah Geological Survey Map, scale 1:62,500.
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Utah G
eological Survey2
Table 1. Summary of sample numbers and locations for U-Pb zircon samples from the Provo and Duchesne 30' x 60' quadrangle areas.Table 1. Summary of sample numbers and locations for U-Pb zircon samples from the Provo and Duchesne 30' x 60' quadrangle areas.
Sample Number Geologic Unit30'x60' quadrangle 7.5' quadrangle
UTM easting NAD27-12
UTM northing NAD27-12
Latitude (°N) WGS84
Longitude (°W) WGS84
Analysis Year Reference
KNC053107-3 Tibble Fm. Provo Granger Mountain 458511 4454797 40.24444 111.48853 2007 Constenius and others, 2011, 2020 in prep.KNC060407-14 Volcanic rocks of East
Traverse Mtns.Provo Timpanogos Cave 443888 4481994 40.48860 111.66284 2007 Constenius and others, 2011, 2020 in prep.
KNC053108-1 North Horn Fm., upper mbr.
Provo Spanish Fork Peak 448590 4435591 40.07086 111.60363 2009 Constenius and others, 2011, 2020 in prep.
KNC071308-2 Uinta Fm., Member C Provo Co-op Creek 487698 4458523 40.27895 111.14543 2009 Constenius and others, 2011, 2020 in prep.KNC070109-1 Duchesne River Fm.,
Starr Flat Mbr.Provo Wolf Creek Summit 498695 4470543 40.38733 111.01610 2010 Constenius and others, 2011, 2020 in prep.
KNC070109-2 Duchesne River Fm., Starr Flat Mbr.
Provo Wolf Creek Summit 498666 4470528 40.38719 111.01644 2010 Constenius and others, 2011, 2020 in prep.
JC 99-37 Lower Ankareh and Upper Thaynes Fms.
Provo Co-op Creek 482450 4466445 40.35023 111.20738 2010 Constenius and others, 2011, 2020 in prep.
KNC61093-2T Tibble Fm. Provo Timpanogos Cave 445724 4481357 40.48299 111.64112 2011 Constenius and others, 2011, 2020 in prep.
KNC101711-1 younger volcaniclastic strata overlying Tvte
Provo Timpanogos Cave 445366 4481071 40.48038 111.64532 2011 Constenius and others, 2011, 2020 in prep.
KNC101811-6 Currant Creek Fm. Duchesne Tabby Mountain 511134 4467295 40.35799 110.86960 2011 Sprinkel, 2018; Sprinkel, 2020 in prep.KNC081612-1 Mesaverde Fm. Duchesne Raspberry Knoll 510830 4468095 40.36520 110.87316 2013 Sprinkel, 2018; Sprinkel, 2020 in prep.KNC081612-2 Mesaverde Fm. Duchesne Tabby Mountain 510777 4468567 40.36945 110.87378 2013 Sprinkel, 2018; Sprinkel, 2020 in prep.
KNC081612-3 Mesaverde Fm. Duchesne Raspberry Knoll 510766 4468595 40.36971 110.87391 2013 Sprinkel, 2018; Sprinkel, 2020 in prep.
KNC081612-5 Mesaverde Fm. Duchesne Tabby Mountain 510633 4468732 40.37094 110.87547 2013 Sprinkel, 2018; Sprinkel, 2020 in prep.
Notes:Samples in the Duchesne 30' x 60' quadrangle were collected by K.N. Constenius.
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3U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
APPENDIX
Arizona LaserChron Center Procedures for 2007 and 2009 Zircon Data
Heavy mineral concentrates of the
-
Utah Geological Survey4
U-Pb geochronologic analyses of detrital zircon (Nu HR ICPMS)
Zircon crystals are extracted from samples by traditional methods of crushing and grinding, followed by separation with a Wilfley table, heavy liquids, and a Frantz magnetic separator. Samples are processed such that all zircons are retained in the final heavy mineral fraction. A large split of these grains (generally thousands of grains) is incorporated into a 1” epoxy mount together with fragments of our Sri Lanka standard zircon. The mounts are sanded down to a depth of ~20 microns, polished, imaged, and cleaned prior to isotopic analysis.
U-Pb geochronology of zircons is conducted by laser ablation multicollector inductively coupled plasma mass spectrometry (LA-MC-ICPMS) at the Arizona LaserChron Center (Gehrels et al., 2006, 2008). The analyses involve ablation of zircon with a Photon Machines Analyte G2 excimer laser (or, prior to May 2011, a New Wave UP193HE Excimer laser) using a spot diameter of 30 microns. The ablated material is carried in helium into the plasma source of a Nu HR ICPMS, which is equipped with a flight tube of sufficient width that U, Th, and Pb isotopes are measured simultaneously. All measurements are made in static mode, using Faraday detectors with 3x1011 ohm resistors for 238U, 232Th, 208Pb-206Pb, and discrete dynode ion counters for 204Pb and 202Hg. Ion yields are ~0.8 mv per ppm. Each analysis consists of one 15-second integration on peaks with the laser off (for backgrounds), 15 one-second integrations with the laser firing, and a 30 second delay to purge the previous sample and prepare for the next analysis. The ablation pit is ~15 microns in depth.
For each analysis, the errors in determining 206Pb/238U and 206Pb/204Pb result in a measurement error of ~1-2% (at 2-sigma level) in the 206Pb/238U age. The errors in measurement of 206Pb/207Pb and 206Pb/204Pb also result in ~1-2% (at 2-sigma level) uncertainty in age for grains that are >1.0 Ga, but are substantially larger for younger grains due to low intensity of the 207Pb signal. For most analyses, the cross-over in precision of 206Pb/238U and 206Pb/207Pb ages occurs at ~1.0 Ga.
204Hg interference with 204Pb is accounted for measurement of 202Hg during laser ablation and subtraction of 204Hg according to the natural 202Hg/204Hg of 4.35. This Hg is correction is not significant for most analyses because our Hg backgrounds are low (generally ~150 cps at mass 204).
Common Pb correction is accomplished by using the Hg-corrected 204Pb and assuming an initial Pb composition from Stacey and Kramers (1975). Uncertainties of 1.5 for 206Pb/204Pb and 0.3 for 207Pb/204Pb are applied to these compositional values based on the variation in Pb isotopic composition in modern crystal rocks.
Inter-element fractionation of Pb/U is generally ~5%, whereas apparent fractionation of Pb isotopes is generally
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5U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
The analytical data are reported in the tables. Uncertainties shown in these tables are at the 1-sigma level, and include only measurement errors. Analyses that are >20% discordant (by comparison of 206Pb/238U and 206Pb/207Pb ages) or >5% reverse discordant (in italics in tables) are not considered further.
The resulting interpreted ages are shown on Pb*/U concordia diagrams and relative age-probability diagrams using the routines in Isoplot (Ludwig, 2008). The age-probability diagrams show each age and its uncertainty (for measurement error only) as a normal distribution, and sum all ages from a sample into a single curve. Composite age probability plots are made from an in-house Excel program (see Analysis Tools for link) that normalizes each curve according to the number of constituent analyses, such that each curve contains the same area, and then stacks the probability curves.
References:
Gehrels, G.E., Valencia, V., Ruiz, J., 2008, Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation–multicollector–inductively coupled plasma–mass spectrometry: Geochemistry, Geophysics, Geosystems, v. 9, Q03017, doi:10.1029/2007GC001805.
Gehrels, G.E., Valencia, V., Pullen, A., 2006, Detrital zircon geochronology by Laser-Ablation Multicollector ICPMS at the Arizona LaserChron Center, in Loszewski, T., and Huff, W., eds., Geochronology: Emerging Opportunities, Paleontology Society Short Course: Paleontology Society Papers, v. 11, 10 p.
Ludwig, K.R., 2008, Isoplot 3.60. Berkeley Geochronology Center, Special Publication No. 4, 77 p.Stacey, J.S., and Kramers, J.D., 1975, Approximation of terrestrial lead isotope evolution by a two stage
model: Earth and Planetary Science Letters, v. 26, p. 207 221.
Notes inserted below data table:
1. Analyses with >10% uncertainty (1-sigma) in 206Pb/238U age are not included.2. Analyses with >10% uncertainty (1-sigma) in 206Pb/207Pb age are not included, unless 206Pb/238U
age is 20% discordance ( 500 Ma and with >5% reverse discordance (
-
Utah Geological Survey6
12. Common Pb composition assigned uncertainties of 1.5 for 206Pb/204Pb, 0.3 for 207Pb/204Pb, and 2.0 for 208Pb/204Pb.
13. U/Pb and 206Pb/207Pb fractionation is calibrated relative to fragments of a large Sri Lanka zircon of 563.5 ± 3.2 Ma (2-sigma).
14. U decay constants and composition as follows: 235U = 9.8485 x 10-10, 238U = 1.55125 x 10-10, 238U/235U = 137.88.
15. Weighted mean and concordia plots determined with Isoplot (Ludwig, 2008).
References:
Gehrels, G.E., Valencia, V., Ruiz, J., 2008, Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation-multicollector-inductively coupled plasma-mass spectrometry: Geochemistry, Geophysics, Geosystems, v. 9, Q03017, doi:10.1029/2007GC001805.
Ludwig, K., 2008, Isoplot 3.6: Berkeley Geochrono9logy Center Special Publication 4, 77 p.Stacey, J.S., and Kramers, J.D., 1975, Approximation of terrestrial lead isotope evolution by a two stage
model: Earth and Planetary Science Letters, v. 26, p. 207-221.
U-Pb geochronologic analyses of igneous zircon (Nu HR ICPMS)
Zircon crystals are extracted from samples by traditional methods of crushing and grinding, followed by separation with a Wilfley table, heavy liquids, and a Frantz magnetic separator. Samples are processed such that all zircons are retained in the final heavy mineral fraction. A split of these grains (generally 50-100 grains) are selected from the grains available and incorporated into a 1” epoxy mount together with fragments of our Sri Lanka standard zircon. The mounts are sanded down to a depth of ~20 microns, polished, imaged, and cleaned prior to isotopic analysis.
U-Pb geochronology of zircons was conducted by laser ablation multicollector inductively coupled plasma mass spectrometry (LA-MC-ICPMS) at the Arizona LaserChron Center (Gehrels et al., 2008). The analyses involve ablation of zircon with a Photon Machines Analyte G2 Excimer laser (or, prior to May 2011, a New Wave UP193HE Excimer laser) using a spot diameter of 30 microns. The ablated material is carried in helium into the plasma source of a Nu HR ICPMS, which is equipped with a flight tube of sufficient width that U, Th, and Pb isotopes are measured simultaneously. All measurements are made in static mode, using Faraday detectors with 3x1011 ohm resistors for 238U, 232Th, 208Pb-206Pb, and discrete dynode ion counters for 204Pb and 202Hg. Ion yields are ~0.8 mv per ppm. Each analysis consists of one 15-second integration on peaks with the laser off (for backgrounds), 15 one-second integrations with the laser firing, and a 30 second delay to purge the previous sample and prepare for the next analysis. The ablation pit is ~15 microns in depth.
For each analysis, the errors in determining 206Pb/238U and 206Pb/204Pb result in a measurement error of ~1-2% (at 2-sigma level) in the 206Pb/238U age. The errors in measurement of 206Pb/207Pb and 206Pb/204Pb also result in ~1-2% (at 2-sigma level) uncertainty in age for grains that are >1.0 Ga, but are substantially larger for younger grains due to low intensity of the 207Pb signal. For most analyses, the cross-over in precision of 206Pb/238U and 206Pb/207Pb ages occurs at ~1.0 Ga.
-
7U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
204Hg interference with 204Pb is accounted for measurement of 202Hg during laser ablation and subtraction of 204Hg according to the natural 202Hg/204Hg of 4.35. This Hg is correction is not significant for most analyses because our Hg backgrounds are low (generally ~150 cps at mass 204).
Common Pb correction is accomplished by using the Hg-corrected 204Pb and assuming an initial Pb composition from Stacey and Kramers (1975). Uncertainties of 1.5 for 206Pb/204Pb and 0.3 for 207Pb/204Pb are applied to these compositional values based on the variation in Pb isotopic composition in modern crystal rocks.
Inter-element fractionation of Pb/U is generally ~5%, whereas apparent fractionation of Pb isotopes is generally 20% discordant (by comparison of 206Pb/238U and 206Pb/207Pb ages) or >5% reverse discordant (in italics in tables) are not considered further.
The resulting interpreted ages are shown on Pb*/U concordia diagrams and weighted mean diagrams using the routines in Isoplot (Ludwig, 2008). The weighted mean diagrams show the weighted mean (weighting according to the square of the internal uncertainties), the uncertainty of the weighted mean, the external (systematic) uncertainty that corresponds to the ages used, the final uncertainty of the age (determined by quadratic addition of the weighted mean and external uncertainties), and the MSWD of the data set.
References:
Gehrels, G.E., Valencia, V., Ruiz, J., 2008, Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation–multicollector–inductively coupled plasma–mass spectrometry: Geochemistry, Geophysics, Geosystems, v. 9, Q03017, doi:10.1029/2007GC001805.
Ludwig, K.R., 2008, Isoplot 3.60. Berkeley Geochronology Center, Special Publication No. 4, 77 p.Stacey, J.S., and Kramers, J.D., 1975, Approximation of terrestrial lead isotope evolution by a two stage
model: Earth and Planetary Science Letters, v. 26, p. 207 221.
Notes inserted below data table:
1. Analyses with >10% uncertainty (1-sigma) in 206Pb/238U age are not included.2. Analyses with >10% uncertainty (1-sigma) in 206Pb/207Pb age are not included, unless 206Pb/238U
age is 20% discordance (
-
Utah Geological Survey8
6. Analyses with 206Pb/238U age > 500 Ma and with >5% reverse discordance (
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9U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
Zircon Images (Cathodoluminescence and Scanning Electron Microscope)
KNC-053107-3200 microns200 microns
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Utah Geological Survey10
KNC-060407-14200 microns200 microns
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11U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
KNC-070109-1(1)
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Utah Geological Survey12
KNC-070109-1(2)
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13U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
KNC-070109-1(3)
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Utah Geological Survey14
KNC-070109-2(1,C)
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15U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
KNC-070109-2(2)
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Utah Geological Survey16
KNC-070109-2(3)
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17U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
Sample JC99-7 no images of zircon grains
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Utah Geological Survey18
KNC-61093-2T(1)
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19U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
KNC-61093-2T(2)
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Utah Geological Survey20
KNC-61093-2T(3)
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21U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah
KNC-101711-1
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Utah Geological Survey22
KNC-101811-6
Lab Data/2007 Zr Data Results Table.docx
U-Pb GEOCHRONOLOGIC DATA FOR
KURT CONSTENIUS 2007-2 SAMPLES
By Victor A. Valencia and George Gehrels
Arizona LaserChron Center
Department of Geosciences
University of Arizona
Tucson, AZ 85721
DECEMBER 2007
RESULTS
Sample
Crystallization
Age (2)
Inherited Age
KNC-53107-3
34.0 +0.5/-0.9 Ma
Concordant ~117 Ma, ~1850 Ma (2), ~2500 Ma (2)
KNC-060407-14
35.6 +0.6/-1.1Ma
Discordia solved at 1068 ± 69 Ma (n=4)
Sample
Maximum Deposition Age (Ma)
Other Peak Ages
KNC-073107-1TL
74 Ma (12)
80 (n=12), 85(10), 92(4), 99(8), 104(6), 161(3), 165(3), 1638(9), 1791(7), 1846(7), 2153(4)
KNC-080207-2
79 Ma (3)
85(n=5), 88(5), 94(5), 98(7), 102(8), 323(3), 396(3), 420 (3), 1071(5), 1651(9), 1794(7), 1875(7), 1912(7), 2001(5), 2794(3).
Other Information as attached -
A data table with characteristics of each analysis (Excel file)
Relevant plots (Excel file)
CL images from the volcanic samples (PDF file)
Please let us know if you need any plots or additional information.
Best Regards,
Victor A Valencia
Lab Data/Constenius data2007-2corrected.xls
Lab Data/Constenius reportDEC2007corrected.doc
U-Pb GEOCHRONOLOGIC DATA FOR
KURT CONSTENIUS 2007-2 SAMPLES
By Victor A Valencia and George Gehrels
Arizona LaserChron Center
Department of Geosciences
University of Arizona
Tucson, AZ 85721
DECEMBER 2007
ANALYTICAL PROCEDURE
Heavy mineral concentrates of the 600 Ma
Check fractionation correction plots (206/238, 206/207, 208/232) and remove "bad" standards (only if necessary) by typing "xx" in column A
Evaluate unknowns: Accept "bad" analyses by typing OK in column AA, Reject analyses by inserting "xx" in column AA
Charts of age versus U/Th, Ucon, and concordance are helpful in evaluating complexities.
Make a concordia diagram of standards from Columns AO-AS
Make a concordia diagram of unknowns from Columns AB-AF
For detrital zircon data, use the concordia diagram to adjust the cutoff between 68 and 67 ages -- cutoff value goes in Cell S1. Default = 900 Ma.
Press "Zircon Datatable" or "Mon Datatable" buttons in Sheet1 to make datatable
G. Gehrels, 14 March, 2010
206238
00.98922660730.99236560440.9860876102
00.9904243180.99325334240.9875952935
0.99777019310.9904243180.99325334240.9875952935
0.98183624960.9904243180.99325334240.9875952935
00.9904243180.99325334240.9875952935
0.98422413010.99402409710.99834556790.9897026264
00.99402409710.99834556790.9897026264
0.98684875170.99402409710.99834556790.9897026264
00.99402409710.99834556790.9897026264
00.99402409710.99834556790.9897026264
00.99363522990.99739788190.9898725779
00.99363522990.99739788190.9898725779
0.99545371210.99363522990.99739788190.9898725779
00.99363522990.99739788190.9898725779
00.99363522990.99739788190.9898725779
00.99432137220.99770991450.9909328299
0.99641287120.99432137220.99770991450.9909328299
00.99432137220.99770991450.9909328299
00.99227718920.99608821320.9884661652
00.99628460231.00003446450.9925347401
1.01562277210.99628460231.00003446450.9925347401
00.99817177241.00193621820.9944073265
00.99817177241.00193621820.9944073265
00.99817177241.00202680910.9943167356
00.99817177241.00202680910.9943167356
0.99091315930.99817177241.00202680910.9943167356
00.99817177241.00202680910.9943167356
00.99951368791.00297600230.9960513735
01.00287519791.00718537880.998565017
01.00315462881.00696092110.9993483365
0.99981051081.00315462881.00696092110.9993483365
01.00315462881.00696092110.9993483365
01.00427825511.00848365421.0000728559
01.00548804991.00931883911.0016572606
1.00826860851.00548804991.00931883911.0016572606
01.00548804991.00931883911.0016572606
01.00379892951.00787725310.9997206058
01.00303647571.00668101440.999391937
0.98570631021.00303647571.00668101440.999391937
01.00303647571.00668101440.999391937
01.00303647571.00668101440.999391937
01.00578447471.00914640781.0024225415
1.00622326551.00578447471.00914640781.0024225415
1.02155189431.00578447471.00914640781.0024225415
1.0048312141.00578447471.00914640781.0024225415
01.00578447471.00914640781.0024225415
01.00696767641.01026695991.003668393
01.00696767641.01026695991.003668393
1.01274681861.00696767641.01026695991.003668393
01.00696767641.01026695991.003668393
01.00675085441.01048066841.0030210404
01.00736555521.01070308151.0040280288
0.99846175311.00743500771.01042339761.0044466179
01.00743500771.01042339761.0044466179
01.00871690131.01080940571.0066243968
01.00871690131.01080940571.0066243968
1.0101491521.00871690131.01080940571.0066243968
01.00871690131.01080940571.0066243968
01.00913250721.01147223081.0067927836
01.00840964491.01021199641.0066072935
01.00930425271.01136531561.0072431898
1.00809292331.00930425271.01136531561.0072431898
01.00930425271.01136531561.0072431898
01.00930425271.01136531561.0072431898
01.00872108361.01097055791.0064716094
01.00872108361.01097055791.0064716094
1.01105375981.00872108361.01097055791.0064716094
1.00792117561.00872108361.01097055791.0064716094
206/238 of standards with 1-sigma std err & 2% error
Analysis
206/238 FRACTIONATION FACTOR
206207
00.99822938290.99926851060.9971902552
00.99897849931.00011032650.9978466721
0.99644605250.99897849931.00011032650.9978466721
0.99672823890.99897849931.00011032650.9978466721
00.99897849931.00011032650.9978466721
1.0013337150.99943536781.00049543970.998375296
00.99943536781.00049543970.998375296
1.00012346670.99943536781.00049543970.998375296
00.99943536781.00049543970.998375296
00.99943536781.00049543970.998375296
00.99864786460.99985739990.9974383294
00.99864786460.99985739990.9974383294
0.99651544150.99864786460.99985739990.9974383294
00.99864786460.99985739990.9974383294
00.99864786460.99985739990.9974383294
00.99810593880.99930241420.9969094633
1.00272408110.99810593880.99930241420.9969094633
00.99810593880.99930241420.9969094633
00.99844132880.99977744950.9971052082
00.99871501741.00003197810.9973980567
1.0021765790.99871501741.00003197810.9973980567
00.99819127790.99963934040.9967432154
00.99819127790.99963934040.9967432154
00.99817283770.99961791460.9967277609
00.99817283770.99961791460.9967277609
0.99313534230.99817283770.99961791460.9967277609
00.99817283770.99961791460.9967277609
00.99893137831.00047228390.9973904726
00.99885788661.00041242610.9973033471
00.99804567730.99955937640.9965319782
0.99377053170.99804567730.99955937640.9965319782
00.99804567730.99955937640.9965319782
00.99726594340.99886398490.9956679019
00.99841300721.0001668260.9966591885
0.99837037050.99841300721.0001668260.9966591885
00.99841300721.0001668260.9966591885
00.99778574530.99971584210.9958556485
00.99829858121.00003311590.9965640466
1.00003126590.99829858121.00003311590.9965640466
00.99829858121.00003311590.9965640466
00.99829858121.00003311590.9965640466
00.99975255411.0014004430.9981046652
1.00529539040.99975255411.0014004430.9981046652
0.99607449150.99975255411.0014004430.9981046652
0.99317242160.99975255411.0014004430.9981046652
00.99975255411.0014004430.9981046652
01.00166362471.00332498611.0000022633
01.00166362471.00332498611.0000022633
1.00714802611.00166362471.00332498611.0000022633
01.00166362471.00332498611.0000022633
01.00221250041.00404704011.0003779608
01.00199074611.00361332991.0003681624
1.0013755971.00191380141.00336533441.0004622684
01.00191380141.00336533441.0004622684
01.0021827351.00379358891.0005718812
01.0021827351.00379358891.0005718812
1.00335023171.0021827351.00379358891.0005718812
01.0021827351.00379358891.0005718812
01.00166395911.00342177850.9999061398
01.00278185271.00461510731.000948598
01.00331226071.00457646031.0020480611
1.00769329771.00331226071.00457646031.0020480611
01.00331226071.00457646031.0020480611
01.00331226071.00457646031.0020480611
01.00203367231.00331514541.0007521992
01.00203367231.00331514541.0007521992
1.00066022041.00203367231.00331514541.0007521992
1.00137518821.00203367231.00331514541.0007521992
206/207 std age with 1-sigma std err & 2% error
Analysis
206/207 FRACTIONATION FACTOR
208232
00.34811425220.36792649650.3283020079
00.3430112310.35997366520.3260487967
0.4251868950.3430112310.35997366520.3260487967
0.31335225330.3430112310.35997366520.3260487967
00.3430112310.35997366520.3260487967
0.34225131610.34734068440.36231604540.3323653235
00.34734068440.36231604540.3323653235
0.33117879670.34734068440.36231604540.3323653235
00.34734068440.36231604540.3323653235
00.34734068440.36231604540.3323653235
00.34432251350.35763812210.331006905
00.34432251350.35763812210.331006905
0.32860200010.34432251350.35763812210.331006905
00.34432251350.35763812210.331006905
00.34432251350.35763812210.331006905
00.34285904740.35469314880.3310249459
0.31749612470.34285904740.35469314880.3310249459
00.34285904740.35469314880.3310249459
00.32897914550.33560458370.3223537073
00.32971854040.33597620080.3234608801
0.3733174050.32971854040.33597620080.3234608801
00.32721198530.33429672570.3201272449
00.32721198530.33429672570.3201272449
00.32447545090.331960240.3169906618
00.32447545090.331960240.3169906618
0.32319531740.32447545090.331960240.3169906618
00.32447545090.331960240.3169906618
00.32512795590.33161388740.3186420243
00.32766017660.33436339770.3209569556
00.32914587370.33509747630.3231942711
0.33115131780.32914587370.33509747630.3231942711
00.32914587370.33509747630.3231942711
00.33108749850.33748956610.3246854309
00.33164640150.33729284050.3259999625
0.32193249450.33164640150.33729284050.3259999625
00.33164640150.33729284050.3259999625
00.32962158090.33289582680.326347335
00.33088461640.33393382870.3278354042
0.31565516180.33088461640.33393382870.3278354042
00.33088461640.33393382870.3278354042
00.33088461640.33393382870.3278354042
00.33382747460.33733593170.3303190176
0.32839048060.33382747460.33733593170.3303190176
0.34379532480.33382747460.33733593170.3303190176
0.33806005590.33382747460.33733593170.3303190176
00.33382747460.33733593170.3303190176
00.33641605720.34079211890.3320399954
00.33641605720.34079211890.3320399954
0.33499981910.33641605720.34079211890.3320399954
00.33641605720.34079211890.3320399954
00.33882998430.34334501390.3343149547
00.34107968970.34545454920.3367048301
0.33846282970.34313360480.34745440890.3388128008
00.34313360480.34745440890.3388128008
00.34523976540.3488030150.3416765159
00.34523976540.3488030150.3416765159
0.34927139570.34523976540.3488030150.3416765159
00.34523976540.3488030150.3416765159
00.34694642310.35024715550.3436456908
00.34757664280.35135376090.3437995247
00.34995578950.35403423950.3458773395
0.35751101080.34995578950.35403423950.3458773395
00.34995578950.35403423950.3458773395
00.34995578950.35403423950.3458773395
00.35378677610.35744813530.350125417
00.35378677610.35744813530.350125417
0.35457792190.35378677610.35744813530.350125417
0.35840482920.35378677610.35744813530.350125417
208/232 of standards with 1-sigma std err & 2% error
Analysis
208/232 FRACTIONATION FACTOR
age vs Uconc
156.1218258388
75.8595610574
521.6833983105
453.706751856
482.5877883997
497.0714979942
492.4882682163
442.2951189812
225.1012592915
351.279954454
236.9854443797
478.6646301325
490.6288578964
283.1838426178
185.4963874992
196.2571376495
575.6508492377
339.7074885284
393.6909778988
277.390264603
592.4400712995
319.3220943048
411.1487964824
238.2598082478
575.8575877119
493.9968340936
229.768943643
233.0511905162
62.275757213
508.7433008375
510.0977222646
151.274946161
251.5775519313
250.2078812205
450.2134597966
224.8518442614
159.812782458
196.3006411041
532.4717973258
150.0456876899
252.3705374873
52.3329538419
503.5022918435
574.4589382236
558.3727389755
224.8246200965
309.0318652364
309.7420299358
531.1592852067
254.4276622726
323.7024012368
298.5099786396
563.845406443
421.6830289751
269.9329104053
314.9013139899
440.1993539163
401.8366619711
289.8881055593
372.8423468135
272.181932131
502.3413732565
576.0119790919
250.6359722037
180.0179942269
486.9177611784
571.8441276391
554.0201254398
Uconc (ppm)
Best age (Ma)
247.5748162256
241.0392692474
247.884998168
254.9985045816
254.6869030042
249.7729253656
242.1772406908
247.6692516628
247.7879624429
251.8557778404
246.7065843185
1475.5603265999
248.4723460632
242.6002440837
1430.3652578539
250.6199824497
251.1837492389
248.8415016731
252.4107101594
253.5155580933
254.5436697329
249.2257689435
249.778109499
528.6763678845
248.8088372377
250.9334222066
247.8981015554
243.1505297066
250.1892719033
250.0457961712
244.8698415866
247.8286125676
255.9061189651
246.3020887723
244.8648087346
253.3393827618
250.0978829401
425.9699344938
426.6092839098
age vs UTh
0.854985204
0.8469416881
0.8852040153
2.3899884971
1.1513802222
1.1890830692
0.8078085943
0.6672567754
0.9611674596
0.9244286458
0.7632480161
2.9827792599
1.0902342521
0.965683455
1.7006571541
1.0642721513
1.0663650345
0.7944345371
0.7134952577
0.9394776991
1.0447227307
1.0356477636
0.8760668692
0.1806210345
1.1269701779
0.9679303359
1.0143536887
0.820180787
0.9301524144
0.6821177308
0.775273488
1.018936898
0.9500162607
0.7400984413
0.9090016754
0.7286024858
0.819164085
1.0918578566
1.3903250864
U/Th
Best age (Ma)
247.5748162256
241.0392692474
247.884998168
254.9985045816
254.6869030042
249.7729253656
242.1772406908
247.6692516628
247.7879624429
251.8557778404
246.7065843185
1475.5603265999
248.4723460632
242.6002440837
1430.3652578539
250.6199824497
251.1837492389
248.8415016731
252.4107101594
253.5155580933
254.5436697329
249.2257689435
249.778109499
528.6763678845
248.8088372377
250.9334222066
247.8981015554
243.1505297066
250.1892719033
250.0457961712
244.8698415866
247.8286125676
255.9061189651
246.3020887723
244.8648087346
253.3393827618
250.0978829401
425.9699344938
426.6092839098
age vs concordance
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
0
Note that discordance filters apply only to analyses with 6/8 age >600 Ma (discordance tough to measure for young analyses)
Concordance (%)
Best age (Ma)
247.5748162256
241.0392692474
247.884998168
254.9985045816
254.6869030042
249.7729253656
242.1772406908
247.6692516628
247.7879624429
251.8557778404
246.7065843185
1475.5603265999
248.4723460632
242.6002440837
1430.3652578539
250.6199824497
251.1837492389
248.8415016731
252.4107101594
253.5155580933
254.5436697329
249.2257689435
249.778109499
528.6763678845
248.8088372377
250.9334222066
247.8981015554
243.1505297066
250.1892719033
250.0457961712
244.8698415866
247.8286125676
255.9061189651
246.3020887723
244.8648087346
253.3393827618
250.0978829401
425.9699344938
426.6092839098
Concordia
0.00197164110.21770750890.48281157730.8056307921.19873017381.67741024282.26030255710000����
0.0098971561����
0.0198922658����
0.0401802339����
0.0608717757����
0.0819749191����
0.1034978518����
0.1254489244����
0.28303940850.14783665360.02329438090.02329438090.00107994820.0010799482
0.26846238640.17066972550.01056003870.01056003870.00079813480.0007981348
0.26361469330.19395699890.02860366060.02860366060.00092810220.0009281022
0.2177075089����
0.2419304704����
0.31598466930.26663528150.03699973090.03699973090.00160567330.0016056733
0.27962516810.29183152730.02081895140.02081895140.00053461410.0005346141
0.28335786110.31752898340.01948503620.01948503620.00089866750.0008986675
0.3437376202����
0.26754777640.37046760620.00895979270.00895979270.00048734460.0004873446
0.28594416320.39772931220.0233164140.0233164140.00085502110.0008550211
0.26901210120.42553331520.01631351350.01631351350.00053484040.0005348404
0.4538904029����
0.28179756640.48281157730.01120496350.01120496350.00119589770.0011958977
0.2736848640.51230805940.01172868180.01172868180.00043372050.0004337205
3.30705498730.54239129340.06093754720.06093754720.00453725110.0045372511
0.573072951����
0.6043649364����
0.26593684650.63627939020.02701018740.02701018740.00050209070.0005020907
0.28274994240.66882869480.02511847780.02511847780.0017966010.001796601
3.13932264140.70202547890.08132790890.08132790890.00193115780.0019311578
0.7358826222����
0.7704132608����
0.27523485450.8056307920.03259426510.03259426510.00173544180.0017354418
0.27510596030.84154887980.01835162570.01835162570.00057017360.0005701736
0.27286316630.87818145960.01598837670.01598837670.00098152870.0009815287
0.9155427446����
0.28577577640.95364723010.01784869980.01784869980.00089324150.0008932415
0.27457588610.99250970010.02779688990.02779688990.00136850230.0013685023
0.28448630321.03214523280.01560678210.01560678210.00067492020.0006749202
1.072569206����
0.25282509151.11379730370.03308865560.03308865560.0012923850.001292385
0.27162197721.15584552160.01709058130.01709058130.00053730380.0005373038
0.65988380061.19873017380.13406695380.13406695380.0026582590.002658259
1.242467899����
1.2870756666����
1.3325707837����
0.27430932111.37897090190.0298832030.0298832030.00100574750.0010057475
0.27072162211.42629402350.02182331340.02182331340.00096480480.0009648048
0.28275619561.47455850920.01936502190.01936502190.00087239960.0008723996
1.523783085����
0.2746936611.5739868490.02067197790.02067197790.00148228040.0014822804
0.28623552181.62518927970.01458590760.01458590760.00088624140.0008862414
0.27873186181.67741024280.01723408390.01723408390.00098353020.0009835302
1.7306699991����
0.26482028521.78498921270.01306176510.01306176510.00078297160.0007829716
0.26604372581.84038895850.02086185620.02086185620.00086800990.0008680099
0.28375393031.89689073070.01913345510.01913345510.00052915810.0005291581
1.9545164513����
0.26462072372.0132884780.01112860050.01112860050.00053294020.0005329402
0.27434852322.07322961350.02233360420.02233360420.00102107850.0010210785
0.27904035662.13436311390.01781955990.01781955990.00086473030.0008647303
0.27649032112.19671269830.02028676860.02028676860.00122977170.0012297717
2.2603025571����
2.3251573623����
0.52744124872.39130227660.01824030530.01824030530.0006801230.000680123
0.49289485752.4587629630.01585040120.01585040120.0010971810.001097181
2.5275655954����
2.597736868����
2.6693040062����
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#NAME?
200
400
600
800
1000
1200
0
0
0
0
207Pb/235U
206Pb/238U
0.0003102981
0.0315112913
0.0640155442
0.097544048
0.1321290782
0.1678039275
0.2046029373
0
0
0
0
0.0015524538
0.0031073177
0.0062242909
0.0093509495
0.0124873236
0.0156334434
0.0187893392
0.0391520493
0.0219550414
0.038099063
0.0251305804
0.0392020513
0.0283159868
0.0315112913
0.0347165247
0.0403494258
0.0379317177
0.0402991394
0.0411569013
0.0395064415
0.0443921066
0.0476373647
0.0382823326
0.0508927069
0.0391672723
0.0541581644
0.0391864087
0.0574337688
0.0607195515
0.0398423629
0.0640155442
0.0390121011
0.0673217785
0.2572116539
0.0706382864
0.0739650998
0.0773022506
0.0392967398
0.080649771
0.0383504652
0.0840076932
0.248428313
0.0873760495
0.0907548724
0.0941441943
0.0396430414
0.097544048
0.0397339666
0.1009544661
0.0393562571
0.1043754814
0.1078071269
0.0399318804
0.1112494357
0.0401101291
0.1147024407
0.0402760252
0.1181661754
0.121640673
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Concordia-log
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#NAME?
200
400
600
800
1000
1200
0
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100
20
10
207Pb/235U
206Pb/238U
0.0003102981
0.0315112913
0.0640155442
0.097544048
0.1321290782
0.1678039275
0.2046029373
0
0
0
0
0.0156334434
0.0031073177
0.0015524538
0.0015524538
0.0031073177
0.0062242909
0.0093509495
0.0124873236
0.0156334434
0.0187893392
0.0391520493
0.0219550414
0.038099063
0.0251305804
0.0392020513
0.0283159868
0.0315112913
0.0347165247
0.0403494258
0.0379317177
0.0402991394
0.0411569013
0.0395064415
0.0443921066
0.0476373647
0.0382823326
0.0508927069
0.0391672723
0.0541581644
0.0391864087
0.0574337688
0.0607195515
0.0398423629
0.0640155442
0.0390121011
0.0673217785
0.2572116539
0.0706382864
0.0739650998
0.0773022506
0.0392967398
0.080649771
0.0383504652
0.0840076932
0.248428313
0.0873760495
0.0907548724
0.0941441943
0.0396430414
0.097544048
0.0397339666
0.1009544661
0.0393562571
0.1043754814
0.1078071269
0.0399318804
0.1112494357
0.0401101291
0.1147024407
0.0402760252
0.1181661754
0.121640673
0.0394182144
0.1251259669
0.0395072775
0.1286220908
0.0854676648
0.1321290782
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0.139175779
0.1427155601
0.0393509906
0.1462663404
0.0396935925
0.1498281541
0.0392041637
0.1534010355
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0.1605801391
0.039573581
0.1641864303
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0.1714326653
0.038716103
0.1750726788
0.0391929617
0.178724003
0.0404959107
0.182386673
0.1860607241
0.0389469078
0.1897461916
0.0387152921
0.193443111
0.0400817042
0.197151518
0.0395588434
0.2008714481
0.2046029373
0.2083460213
0.0683106682
0.2121007364
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0.2158671185
0.2196452039
0.2234350291
0.2272366305
DATA
Sheet1
SLstdC:\Users\lab\Desktop\CONSTENSIUS 2010\JC99-37drive:\folder200204 cps1068err1067err0.0430disc5rev1.06/4 fact900cutoff1.068 SE0.867 SE3.882 SEOK or xxSAMPLE CONCORDIAAGESSTD CONCORDIA564.33.00.00.0CORRECTED CONCENTRATIONS AND RATIOSAGES & 1-S SD RANDOM ERRORS0.980.793.85U/Th2062381.0012062382062070.3413208232206204206204207204208204STANDARD VALUES23388656.85561955076.59616concavg 68 age±avg 68 age±min agemax age0.21770750890.48281157730.8056307921.19873017381.67741024282.260302557100000.10349785180.01989226580.0098971561
sampleserial202 (cps)204 (cps)206 (cps)207 (cps)208 (cps)232 (cps)238 (cps)20623868 ± %m6820620767 ± %20620464 ± %20823282 ± %20820484 ± %6/8 age± (Ma)6/7 age± (Ma)8/2 age± (Ma)comment7/5 ratio±(%)6/8 ratio±(%)errcorr6/8 age±(Ma)6/7 age±(Ma)BEST AGE±(Ma)8/2 age±(Ma)7/5 ratio±(%)6/8 ratio±(%)errcorr6/8 age±(Ma)6/7 age±(Ma)sampleU (ppm)Th(ppm)6/4c8/4 ratioU/Th6/7 ratio±(%)8/2 ratio±(%)7/5 ratio±(%)6/8 ratio±(%)errcorr6/8 age±(Ma)7/5 age±(Ma)6/7 age±(Ma)8/2 age±(Ma)BEST AGE±(Ma)%s-err 6/8%s-err 6/7%s-err 8/26/8age68 ff68 ff sw68sw se68 ff +se68 ff - se68 fc bc68 m err %68 64 err %68 pbc err %std fcstd fc swstd swse67 ff +se67 ff - se67 fc bc67 re %67 64 err %67 pbc err %std fcstd fc swstd swse82 ff +se82 ff - se82 fc bc82 re %82 84 err %82 pbc err %0.040905132920623820620720823264c67c68c(%)0327.06.60.00.002000207/5 ratio±(%)6/8 ratio±(%)20040060080010001200000010020100.03151129130.06401554420.0975440480.13212907820.16780392750.204602937300000.01563344340.00310731770.0015524538
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xx40435.893485326455198692080034316934251990.038702035.42-5.018.66489.2154861360.13841442.00545942426256008733820high 6/8 err0.000000.00.000000.00.000.00.00.00.00.00.00.00.00.000000.00.000000.00.000.00.00.00.0xx762154865453.78.84489.220.04415442.020.595552037.380.038202035.421.00241.76256.3474.40.0008733820000.0000.0000.0002420.00.00.0000.9900.00280.9930.9880.038202035.420.004130.000000.0000.9990.00111.00010.99788.84489.221.260.030.00000.34300.01700.36000.32600.04415442.015683.528010.393355486018.3715.6138.19000.0000.0050.00989715610.0015524538100.00000.000.00000.00
std40435.89472321147031244651393422032792235549690.091672.230.0917.0011.44127652650.0668119.459927555601200456880.000000.00.000000.00.000.00.00.00.00.00.00.00.00.735552.70.090782.20.84560.112.00.00.0std52212312765299274.317.0161.450.0228319.450.735552.660.090782.230.84560.112.0559.811.40045688000.0000.0000.0005600.00.00.9980.9900.00280.9930.9880.090782.230.000290.000000.9960.9990.00111.00010.997817.0161.450.080.000.42520.34300.01700.36000.32600.0228319.450090.135210.020221276520.093337819217.8315.5537.5823554969.09333332032791.86720.0000.010.01989226580.0031073177200.00000.000.00000.00
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