u-pb zircon geochronology results from the provo and ...11. common pb correction is from measured...

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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. Constenius 1 , 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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  • 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.

  • Blank pages are intentional for printing purposes.

  • 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.

  • 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.

  • 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

  • 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 (

  • 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

  • Utah Geological Survey10

    KNC-060407-14200 microns200 microns

  • 11U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah

    KNC-070109-1(1)

  • Utah Geological Survey12

    KNC-070109-1(2)

  • 13U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah

    KNC-070109-1(3)

  • Utah Geological Survey14

    KNC-070109-2(1,C)

  • 15U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah

    KNC-070109-2(2)

  • Utah Geological Survey16

    KNC-070109-2(3)

  • 17U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah

    Sample JC99-7 no images of zircon grains

  • Utah Geological Survey18

    KNC-61093-2T(1)

  • 19U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah

    KNC-61093-2T(2)

  • Utah Geological Survey20

    KNC-61093-2T(3)

  • 21U-Pb Zircon geochronology results from the Provo and Duchesne 30' x 60' quadrangles, Utah

    KNC-101711-1

  • 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

    [email protected]

    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

    [email protected]

    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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    0.0395072775

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    0.0396935925

    0.1498281541

    0.0392041637

    0.1534010355

    0.156985019

    0.0384391058

    0.1605801391

    0.039573581

    0.1641864303

    0.0395504438

    0.1678039275

    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

    0.0684166275

    0.2158671185

    0.2196452039

    0.2234350291

    0.2272366305

    Concordia-log

    0.00197164110.21770750890.48281157730.8056307921.19873017381.67741024282.260302557100000.10349785180.01989226580.0098971561����

    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����

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    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����

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    #NAME?

    200

    400

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    0

    0

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    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

    0.135646963

    0.139175779

    0.1427155601

    0.0393509906

    0.1462663404

    0.0396935925

    0.1498281541

    0.0392041637

    0.1534010355

    0.156985019

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    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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