Rioux, Matthew; Bowring, Samuel A; Cheadle, Michael J; John, Barbara E (2016): (Table 2) Zircons analyses from tonalite and oxide gabbro of the mid-ocean ridge from ODP Hole 176-735B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.856807, In supplement to: Rioux, M et al. (2015): Evidence for initial excess 231Pa in mid-ocean ridge zircons. Chemical Geology, 397, 143-156, https://doi.org/10.1016/j.chemgeo.2015.01.011
Always quote citation above when using data! You can download the citation in several formats below.
Further details:
Hiess, Joe; Condon, Daniel J; McLean, Noah; Noble, Stephen R (2012): 238U/235U Systematics in Terrestrial Uranium-Bearing Minerals. Science, 335(6076), 1610-1614, https://doi.org/10.1126/science.1215507
Jaffey, A H; Flynn, K F; Glendenin, L E; Bentley, W C; Essling, A M (1971): Precision measurement of half-lives and specific activities of 235U and 238U. Physical Review C, 4(5), 1889-1906, https://doi.org/10.1103/PhysRevC.4.1889
McLean, N M; Bowring, James F; Bowring, Samuel A (2011): An algorithm for U-Pb isotope dilution data reduction and uncertainty propagation. Geochemistry, Geophysics, Geosystems, 12(6), n/a-n/a, https://doi.org/10.1029/2010GC003478
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -32.723210 * Longitude: 57.266010
Date/Time Start: 1997-10-24T13:45:00 * Date/Time End: 1997-12-01T19:00:00
Minimum DEPTH, sediment/rock: 571 m * Maximum DEPTH, sediment/rock: 854 m
Event(s):
176-735B * Latitude: -32.723210 * Longitude: 57.266010 * Date/Time Start: 1997-10-24T13:45:00 * Date/Time End: 1997-12-01T19:00:00 * Elevation: -720.6 m * Penetration: 1508 m * Recovery: 865.99 m * Location: Indian Ocean * Campaign: Leg176 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 122 cores; 1003.2 m cored; 504.8 m drilled; 86.3 % recovery
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Sample code/label | Sample label | Rioux, Matthew | DSDP/ODP/IODP sample designation | ||
2 | DEPTH, sediment/rock | Depth sed | m | Rioux, Matthew | Geocode | |
3 | Sample ID | Sample ID | Rioux, Matthew | |||
4 | Minerals | Minerals | Rioux, Matthew | |||
5 | Ratio | Ratio | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Ratio of radiogenic to common Pb. | |
6 | Lead | Pb | pg | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Total radiogenic Pb, common Pb and U. |
7 | Standard deviation | Std dev | ± | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Of total radiogenic Pb, common Pb and U. |
8 | Thorium/Uranium ratio | Th/U | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Th/U ratio calculated from 208Pb/206Pb and the 206Pb/238U date of the sample. | |
9 | Lead-206/Lead-204 ratio | 206Pb/204Pb | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Fractionation and spike corrected isotopic ratios, reduced using EARTHTIME ET535 tracer calibration v.3. | |
10 | Lead-206/Lead-204 ratio, error | 206Pb/204Pb e | ± | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Fractionation and spike corrected isotopic ratios, reduced using EARTHTIME ET535 tracer calibration v.3. |
11 | Lead-206/Uranium-238 ratio | 206Pb/238U | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. | |
12 | Lead-206/Uranium-238, error, relative | 206Pb/238U e rel | % | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. |
13 | Lead-207/Uranium-235 ratio | 207Pb/235U | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. | |
14 | Lead-207/Uranium-235, error, relative | 207Pb/235U e rel | % | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. |
15 | Lead-207/Lead-206 ratio | 207Pb/206Pb | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. | |
16 | Lead-207/Lead-206, error, relative | 207Pb/206Pb e rel | % | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. |
17 | Correlation coefficient, isotope ratio error | Rho | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected correlation coefficient of radiogenic 207Pb*/235U and 206Pb*/238U. | |
18 | Age, mineral | Age mineral | Ma | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
19 | Standard deviation | Std dev | ± | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
20 | Age, mineral | Age mineral | Ma | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
21 | Standard deviation | Std dev | ± | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
22 | Age, mineral | Age mineral | Ma | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
23 | Standard deviation | Std dev | ± | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
24 | Discordance | D | % | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Uncorrected: 100 - (100 *(206Pb/238U date)/(207Pb/206Pb date)). |
25 | Lead-206/Uranium-238 ratio | 206Pb/238U | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Th-corrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. | |
26 | Lead-206/Uranium-238, error, relative | 206Pb/238U e rel | % | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Th-corrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. |
27 | Lead-207/Lead-206 ratio | 207Pb/206Pb | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Th-corrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. | |
28 | Lead-207/Lead-206, error, relative | 207Pb/206Pb e rel | % | Rioux, Matthew | Thermal Ionization Mass Spectrometry (TIMS) | Th-corrected fractionation, spike and blank corrected radiogenic isotope ratios. Laboratory blanks were corrected using 206Pb/204Pb = 18.638 ± 0.707, 207Pb/204Pb = 15.494 ± 0.449, 208Pb/204Pb = 37.748 ± 1.227. |
29 | Correlation coefficient, isotope ratio error | Rho | Rioux, Matthew | Calculated | Th-corrected correlation coefficient of radiogenic 207Pb*/235U and 206Pb*/238U. | |
30 | Age, mineral | Age mineral | Ma | Rioux, Matthew | Calculated | Th-corrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
31 | Standard deviation | Std dev | ± | Rioux, Matthew | Calculated | Th-corrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
32 | Age, mineral | Age mineral | Ma | Rioux, Matthew | Calculated | Th-corrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
33 | Standard deviation | Std dev | ± | Rioux, Matthew | Calculated | Th-corrected dates using: 238U / 235U = 137.818 (Hiess et al., 2012; doi: 10.1126/science.1215507), and decay constants of 238U = 1.5513 * 10**-10 yr**-1 and 235U = 9.8485 * 10**-10 yr**-1 (Jaffey et al., 1971; doi:10.1103/PhysRevC.4.1889). |
34 | Discordance | D | % | Rioux, Matthew | Calculated | Th-corrected: 100 - (100 *(206Pb/238U date)/(207Pb/206Pb date)). |
35 | Protactinium-231/Uranium-235 ratio | 231Pa/235U | Rioux, Matthew | Calculated | Calculated initial conditionsafter McLean et al. (2011; doi:10.1029/2010GC003478). | |
36 | Protactinium-231/Uranium-235 ratio, standard deviation | 231Pa/235U std dev | ± | Rioux, Matthew | Calculated | Calculated initial conditions after McLean et al. (2011; doi:10.1029/2010GC003478). |
37 | Protactinium-231/Uranium-235 ratio | 231Pa/235U | Rioux, Matthew | Calculated | (231Pa)/(235U)magma = 2.52 Zircon DPa/DU, calculated initial conditions after McLean et al. (2011; doi:10.1029/2010GC003478). | |
38 | Protactinium-231/Uranium-235 ratio, standard deviation | 231Pa/235U std dev | ± | Rioux, Matthew | Calculated | (231Pa)/(235U)magma = 2.52 Zircon DPa/DU, calculated initial conditions after McLean et al. (2011; doi:10.1029/2010GC003478). |
39 | Protactinium-231/Uranium-235 ratio | 231Pa/235U | Rioux, Matthew | Calculated | (231Pa)/(235U)magma = 1.00 Zircon DPa/DU, calculated initial conditions after McLean et al. (2011; doi:10.1029/2010GC003478). | |
40 | Protactinium-231/Uranium-235 ratio, standard deviation | 231Pa/235U std dev | ± | Rioux, Matthew | Calculated | (231Pa)/(235U)magma = 1.00 Zircon DPa/DU, calculated initial conditions after McLean et al. (2011; doi:10.1029/2010GC003478). |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
780 data points
Data
1 Sample label (DSDP/ODP/IODP sample designation) | 2 Depth sed [m] | 3 Sample ID | 4 Minerals | 5 Ratio (Ratio of radiogenic to common...) | 6 Pb [pg] (Total radiogenic Pb, common P...) | 7 Std dev [±] (Of total radiogenic Pb, commo...) | 8 Th/U (Th/U ratio calculated from 20...) | 9 206Pb/204Pb (Fractionation and spike corre...) | 10 206Pb/204Pb e [±] (Fractionation and spike corre...) | 11 206Pb/238U (Uncorrected fractionation, sp...) | 12 206Pb/238U e rel [%] (Uncorrected fractionation, sp...) | 13 207Pb/235U (Uncorrected fractionation, sp...) | 14 207Pb/235U e rel [%] (Uncorrected fractionation, sp...) | 15 207Pb/206Pb (Uncorrected fractionation, sp...) | 16 207Pb/206Pb e rel [%] (Uncorrected fractionation, sp...) | 17 Rho (Uncorrected correlation coeff...) | 18 Age mineral [Ma] (Uncorrected dates using: 238U...) | 19 Std dev [±] (Uncorrected dates using: 238U...) | 20 Age mineral [Ma] (Uncorrected dates using: 238U...) | 21 Std dev [±] (Uncorrected dates using: 238U...) | 22 Age mineral [Ma] (Uncorrected dates using: 238U...) | 23 Std dev [±] (Uncorrected dates using: 238U...) | 24 D [%] (Uncorrected: 100 - (100 *(206...) | 25 206Pb/238U (Th-corrected fractionation, s...) | 26 206Pb/238U e rel [%] (Th-corrected fractionation, s...) | 27 207Pb/206Pb (Th-corrected fractionation, s...) | 28 207Pb/206Pb e rel [%] (Th-corrected fractionation, s...) | 29 Rho (Th-corrected correlation coef...) | 30 Age mineral [Ma] (Th-corrected dates using: 238...) | 31 Std dev [±] (Th-corrected dates using: 238...) | 32 Age mineral [Ma] (Th-corrected dates using: 238...) | 33 Std dev [±] (Th-corrected dates using: 238...) | 34 D [%] (Th-corrected: 100 - (100 *(20...) | 35 231Pa/235U (Calculated initial conditions...) | 36 231Pa/235U std dev [±] (Calculated initial conditions...) | 37 231Pa/235U ((231Pa)/(235U)magma = 2.52 Zi...) | 38 231Pa/235U std dev [±] ((231Pa)/(235U)magma = 2.52 Zi...) | 39 231Pa/235U ((231Pa)/(235U)magma = 1.00 Zi...) | 40 231Pa/235U std dev [±] ((231Pa)/(235U)magma = 1.00 Zi...) |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
176-735B-99R-4,108-114 | 571 | iz1 | Tonalite | 59.0 | 16.90 | 0.00029 | 0.550 | 3513.83 | 0.177 | 0.0018386 | 0.088 | 0.012164 | 0.323 | 0.048000 | 0.295 | 0.429 | 11.8420 | 0.0100 | 12.276 | 0.039 | 98.4 | 7.0 | 88.0 | 0.0018520 | 0.109 | 0.047660 | 0.302 | 0.341 | 11.9280 | 0.013 | 81.1 | 7.2 | 85.3 | 8.47 | 0.89 | 3.36 | 0.180 | 8.47 | 0.45 |
176-735B-99R-4,108-114 | 571 | iz2 | Tonalite | 45.9 | 12.60 | 0.00027 | 0.610 | 2691.49 | 0.197 | 0.0018394 | 0.075 | 0.012218 | 0.388 | 0.048200 | 0.365 | 0.374 | 11.8463 | 0.0089 | 12.330 | 0.048 | 107.9 | 8.7 | 89.0 | 0.0018524 | 0.104 | 0.047860 | 0.373 | 0.265 | 11.9300 | 0.012 | 91.2 | 8.9 | 86.9 | 9.60 | 1.10 | 3.80 | 0.210 | 9.59 | 0.53 |
176-735B-99R-4,108-114 | 571 | iz3 | Tonalite | 91.6 | 28.58 | 0.00031 | 0.608 | 5358.45 | 0.196 | 0.0018389 | 0.073 | 0.012094 | 0.229 | 0.047721 | 0.197 | 0.526 | 11.8437 | 0.0087 | 12.207 | 0.028 | 84.4 | 4.7 | 86.0 | 0.0018520 | 0.103 | 0.047390 | 0.211 | 0.370 | 11.9270 | 0.012 | 67.6 | 5.1 | 82.4 | 6.99 | 0.65 | 2.77 | 0.130 | 6.99 | 0.33 |
176-735B-99R-4,108-114 | 571 | iz7 | Tonalite | 50.2 | 12.84 | 0.00026 | 0.559 | 2986.15 | 0.180 | 0.0018380 | 0.070 | 0.012028 | 0.364 | 0.047480 | 0.339 | 0.418 | 11.8377 | 0.0083 | 12.140 | 0.044 | 72.5 | 8.1 | 83.7 | 0.0018513 | 0.097 | 0.047140 | 0.346 | 0.299 | 11.9230 | 0.011 | 55.3 | 8.3 | 78.4 | 5.64 | 0.97 | 2.24 | 0.190 | 5.64 | 0.49 |
176-735B-99R-4,108-114 | 571 | z1 | Tonalite | 83.9 | 22.38 | 0.00027 | 0.544 | 4994.11 | 0.175 | 0.0018389 | 0.074 | 0.012166 | 0.238 | 0.048003 | 0.207 | 0.514 | 11.8434 | 0.0088 | 12.278 | 0.029 | 98.4 | 5.0 | 88.0 | 0.0018523 | 0.098 | 0.047650 | 0.217 | 0.383 | 11.9300 | 0.012 | 81.1 | 5.2 | 85.3 | 8.47 | 0.67 | 3.36 | 0.130 | 8.47 | 0.34 |
176-735B-99R-4,108-114 | 571 | z2 | Tonalite | 149.3 | 45.12 | 0.00030 | 0.552 | 8851.79 | 0.178 | 0.0018409 | 0.068 | 0.012131 | 0.169 | 0.047815 | 0.127 | 0.697 | 11.8565 | 0.0081 | 12.244 | 0.021 | 89.1 | 3.1 | 86.7 | 0.0018543 | 0.094 | 0.047470 | 0.143 | 0.497 | 11.9430 | 0.011 | 71.9 | 3.5 | 83.4 | 7.46 | 0.50 | 2.96 | 0.100 | 7.46 | 0.25 |
176-735B-99R-4,108-114 | 571 | z3 | Tonalite | 181.1 | 47.68 | 0.00026 | 0.589 | 10634.69 | 0.190 | 0.0018400 | 0.064 | 0.012107 | 0.156 | 0.047745 | 0.112 | 0.740 | 11.8504 | 0.0075 | 12.220 | 0.019 | 85.6 | 2.8 | 86.2 | 0.0018531 | 0.094 | 0.047406 | 0.133 | 0.493 | 11.9350 | 0.011 | 68.7 | 3.3 | 82.6 | 7.11 | 0.47 | 2.82 | 0.094 | 7.11 | 0.24 |
176-735B-99R-4,108-114 | 571 | z4 | Tonalite | 61.1 | 22.16 | 0.00036 | 0.564 | 3620.57 | 0.182 | 0.0018402 | 0.063 | 0.012132 | 0.299 | 0.047830 | 0.275 | 0.445 | 11.8521 | 0.0075 | 12.244 | 0.036 | 90.0 | 6.6 | 86.8 | 0.0018535 | 0.092 | 0.047490 | 0.283 | 0.302 | 11.9380 | 0.011 | 72.9 | 6.8 | 83.6 | 7.57 | 0.82 | 3.01 | 0.160 | 7.57 | 0.41 |
176-735B-99R-4,108-114 | 571 | z5 | Tonalite | 54.1 | 18.25 | 0.00034 | 0.595 | 3184.11 | 0.192 | 0.0018401 | 0.072 | 0.012098 | 0.348 | 0.047710 | 0.329 | 0.348 | 11.8509 | 0.0085 | 12.210 | 0.042 | 83.7 | 7.8 | 85.8 | 0.0018532 | 0.101 | 0.047370 | 0.337 | 0.243 | 11.9350 | 0.012 | 66.8 | 8.1 | 82.1 | 6.90 | 0.94 | 2.74 | 0.190 | 6.90 | 0.47 |
176-735B-99R-4,108-114 | 571 | iz4 | Tonalite | 14.9 | 8.23 | 0.00055 | 0.563 | 900.11 | 0.182 | 0.0018409 | 0.114 | 0.012180 | 1.129 | 0.048020 | 1.101 | 0.285 | 11.8560 | 0.0140 | 12.300 | 0.140 | 99.0 | 26.0 | 88.1 | 0.0018542 | 0.131 | 0.047680 | 1.104 | 0.240 | 11.9420 | 0.016 | 82.0 | 26.0 | 85.5 | 8.60 | 3.00 | 3.42 | 0.590 | 8.60 | 1.50 |
176-735B-99R-4,108-114 | 571 | iz5 | Tonalite | 3.7 | 1.10 | 0.00030 | 0.510 | 238.97 | 0.165 | 0.0018366 | 0.341 | 0.012160 | 4.508 | 0.048000 | 4.425 | 0.278 | 11.8280 | 0.0400 | 12.270 | 0.550 | 100.0 | 105.0 | 88.1 | 0.0018502 | 0.341 | 0.047700 | 4.429 | 0.267 | 11.9160 | 0.041 | 82.0 | 105.0 | 85.5 | 9.00 | 12.00 | 3.40 | 2.300 | 8.60 | 5.90 |
176-735B-99R-4,108-114 | 571 | iz6 | Tonalite | 8.2 | 2.29 | 0.00028 | 0.546 | 502.64 | 0.176 | 0.0018407 | 0.166 | 0.012300 | 2.065 | 0.048480 | 2.022 | 0.297 | 11.8550 | 0.0200 | 12.410 | 0.250 | 122.0 | 48.0 | 90.2 | 0.0018542 | 0.176 | 0.048130 | 2.024 | 0.269 | 11.9417 | 0.021 | 104.4 | 47.9 | 88.6 | 11.10 | 5.50 | 4.40 | 1.100 | 11.07 | 2.74 |
176-735B-137R-2,71-75 | 854 | iz2 | Oxide gabbro | 9.1 | 3.42 | 0.00038 | 0.650 | 542.21 | 0.209 | 0.0018396 | 0.156 | 0.012180 | 2.004 | 0.048040 | 1.961 | 0.312 | 11.8480 | 0.0180 | 12.290 | 0.240 | 100.0 | 46.0 | 88.1 | 0.0018523 | 0.172 | 0.047700 | 1.964 | 0.273 | 11.9300 | 0.021 | 84.0 | 47.0 | 85.7 | 8.70 | 5.30 | 3.50 | 1.000 | 8.70 | 2.60 |
176-735B-137R-2,71-75 | 854 | iz7 | Oxide gabbro | 7.3 | 2.64 | 0.00036 | 0.432 | 464.58 | 0.139 | 0.0018359 | 0.180 | 0.012290 | 2.192 | 0.048600 | 2.148 | 0.284 | 11.8240 | 0.0210 | 12.400 | 0.270 | 126.0 | 51.0 | 90.6 | 0.0018500 | 0.185 | 0.048200 | 2.150 | 0.267 | 11.9150 | 0.022 | 108.0 | 51.0 | 88.9 | 11.40 | 5.80 | 4.50 | 1.200 | 11.40 | 2.90 |
176-735B-137R-2,71-75 | 854 | iz8 | Oxide gabbro | 8.7 | 3.84 | 0.00044 | 0.645 | 523.39 | 0.208 | 0.0018375 | 0.154 | 0.011920 | 2.036 | 0.047080 | 1.999 | 0.270 | 11.8350 | 0.0180 | 12.030 | 0.240 | 52.0 | 48.0 | 77.3 | 0.0018503 | 0.170 | 0.046760 | 2.002 | 0.235 | 11.9170 | 0.020 | 36.0 | 48.0 | 66.6 | 3.50 | 5.20 | 1.40 | 1.000 | 3.50 | 2.60 |
176-735B-137R-2,71-75 | 854 | iz12 | Oxide gabbro | 8.9 | 4.33 | 0.00049 | 0.906 | 498.07 | 0.292 | 0.0018389 | 0.174 | 0.011960 | 2.249 | 0.047200 | 2.193 | 0.351 | 11.8440 | 0.0210 | 12.070 | 0.270 | 57.0 | 52.0 | 79.2 | 0.0018500 | 0.203 | 0.046900 | 2.198 | 0.292 | 11.9150 | 0.024 | 43.0 | 53.0 | 72.0 | 4.30 | 5.80 | 1.70 | 1.200 | 4.30 | 2.90 |
176-735B-137R-2,71-75 | 854 | iz11 | Oxide gabbro | 4.9 | 3.97 | 0.00082 | 0.772 | 290.79 | 0.249 | 0.0018417 | 0.276 | 0.012190 | 3.584 | 0.048000 | 3.523 | 0.257 | 11.8620 | 0.0330 | 12.300 | 0.440 | 100.0 | 83.0 | 88.1 | 0.0018537 | 0.288 | 0.047700 | 3.527 | 0.237 | 11.9390 | 0.034 | 84.0 | 84.0 | 85.8 | 8.80 | 9.40 | 3.50 | 1.900 | 8.80 | 4.70 |
176-735B-137R-2,71-75 | 854 | iz16 | Oxide gabbro | 5.1 | 1.89 | 0.00037 | 0.546 | 317.80 | 0.176 | 0.0018424 | 0.344 | 0.012350 | 4.372 | 0.048700 | 4.193 | 0.547 | 11.8660 | 0.0410 | 12.470 | 0.540 | 130.0 | 99.0 | 90.9 | 0.0018558 | 0.344 | 0.048300 | 4.199 | 0.532 | 11.9520 | 0.041 | 113.0 | 99.0 | 89.4 | 12.00 | 12.00 | 4.80 | 2.300 | 12.10 | 5.80 |
176-735B-137R-2,71-75 | 854 | iz22 | Oxide gabbro | 7.0 | 4.16 | 0.00059 | 0.604 | 428.63 | 0.195 | 0.0018397 | 0.198 | 0.012020 | 2.493 | 0.047400 | 2.441 | 0.297 | 11.8490 | 0.0230 | 12.130 | 0.300 | 69.0 | 58.0 | 82.8 | 0.0018528 | 0.208 | 0.047100 | 2.444 | 0.273 | 11.9330 | 0.025 | 52.0 | 58.0 | 77.0 | 5.30 | 6.50 | 2.10 | 1.300 | 5.30 | 3.20 |
176-735B-137R-2,71-75 | 854 | iz23 | Oxide gabbro | 4.3 | 1.31 | 0.00031 | 0.653 | 265.59 | 0.210 | 0.0018409 | 0.331 | 0.012400 | 4.277 | 0.048900 | 4.166 | 0.368 | 11.8560 | 0.0390 | 12.510 | 0.530 | 141.0 | 98.0 | 91.6 | 0.0018536 | 0.335 | 0.048500 | 4.170 | 0.352 | 11.9380 | 0.040 | 125.0 | 98.0 | 90.4 | 13.00 | 11.00 | 5.30 | 2.300 | 13.30 | 5.70 |