The Geological
Timescale Versus Radiometric Dating
By
Paul Nethercott
October 2014
The Siderian Period
2,500 To 2,800 Million Years Ago
1. Temporal Evolution of the Lithospheric Mantle,
Journal Of Petrology, 2009, Volume 50, Number 10, Pages 1857-1898
|
Sample |
147Sm/144Nd |
176Lu/176Hf |
187Re/188Os |
187Re/188Os |
187Os/188Os |
|
PL01 |
364 |
-244 |
230 |
360 |
-45 |
|
PL02 |
347 |
-423 |
1,080 |
1,340 |
888 |
|
PL03 |
408 |
-722 |
40 |
70 |
-263 |
|
PL03-L |
406 |
-865 |
150 |
-30 |
-166 |
|
PL06 |
-457 |
-153 |
140 |
320 |
-150 |
|
PL07 |
76 |
-159 |
20 |
-296 |
|
|
PL11 |
601 |
1377 |
270 |
360 |
-4 |
|
PL12 |
128 |
-1 |
930 |
1,290 |
727 |
|
PL13 |
428 |
199 |
-280 |
-380 |
-603 |
|
PL14 |
1,794 |
-1,779 |
-80 |
-120 |
-389 |
|
PL15 |
232 |
-2,614 |
840 |
1,100 |
623 |
|
PL15-L |
362 |
4,192 |
840 |
1,100 |
623 |
|
PL16 |
425 |
-143 |
150 |
180 |
-135 |
|
PL17 |
881 |
2,285 |
160 |
220 |
-124 |
|
PL17-L |
847 |
1,740 |
230 |
310 |
-48 |
|
PL18 |
384 |
1390 |
-1,720 |
1,230 |
|
|
PL19 |
162 |
1,227 |
-10 |
-40 |
-318 |
|
PL19-L |
14 |
1,345 |
250 |
380 |
-27 |
|
PL19-LR |
42 |
1,308 |
230 |
470 |
-50 |
|
PL23 |
1,412 |
1,424 |
990 |
1,130 |
798 |
|
PL23-L |
967 |
1,895 |
920 |
1,040 |
719 |
|
SW01 |
878 |
492 |
-930 |
470 |
-1,366 |
2. Diamonds And Mantle-Derived Xenoliths,
Earth and Planetary Science Letters, Volume 42, 1979, Pages 58-70
|
87Rb/86Sr |
Pb207/Pb206 |
|
91,957 |
5,249 |
|
53,584 |
5,231 |
|
51,582 |
5,097 |
|
43,201 |
5,053 |
|
33,542 |
5,040 |
|
24,366 |
4,953 |
|
18,139 |
4,944 |
|
17,036 |
4,934 |
|
15,716 |
4,919 |
|
15,340 |
4,913 |
|
13,633 |
4,910 |
|
12,202 |
4,904 |
|
4,450 |
4,898 |
|
3,257 |
4,885 |
3. Temporal Evolution of the Lithospheric Mantle,
Journal Of Petrology, 2009, Volume 50, Number 10, Pages 1857-1898
|
Sample |
187Os/188Os |
187Re/188Os |
187Re/188Os |
87Rb/86Sr |
147Sm/144Nd |
176Lu/176Hf |
|
SW03 |
680 |
890 |
1,410 |
22 |
-128 |
-660 |
|
SW04 |
390 |
630 |
750 |
17 |
400 |
1011 |
|
SW05 |
-1,643 |
-1,210 |
2,120 |
14 |
179 |
-1457 |
|
SW06 |
164 |
430 |
780 |
|
|
|
|
SW07 |
487 |
770 |
-280 |
16 |
331 |
-236 |
|
SW07 |
469 |
700 |
780 |
|
|
|
|
SW08 |
-364 |
-40 |
-410 |
17 |
405 |
1028 |
|
SW09 |
565 |
790 |
1,280 |
16 |
346 |
-218 |
|
SW09 |
503 |
730 |
850 |
|
|
|
|
SW10 |
199 |
470 |
2,510 |
17 |
334 |
380 |
|
SW11 |
631 |
850 |
1,390 |
17 |
-2301 |
-1982 |
|
SW12 |
-757 |
-390 |
890 |
17 |
259 |
133 |
|
SW13 |
367 |
620 |
4,020 |
16 |
193 |
852 |
|
SW14 |
2 |
290 |
1,440 |
20 |
150 |
1097 |
|
SW15 |
619 |
840 |
2,410 |
17 |
370 |
-2121 |
|
SW16 |
852 |
1,050 |
1,630 |
21 |
123 |
1543 |
|
SW17 |
313 |
560 |
900 |
21 |
336 |
-12 |
|
SW18 |
25 |
310 |
-11,060 |
|
-3742 |
-9369 |
|
SW18 |
-17 |
270 |
20,710 |
|
|
|
|
SW19 |
27 |
300 |
490 |
10 |
-281 |
-1614 |
|
SW20 |
902 |
1,100 |
2,570 |
15 |
194 |
870 |
|
SW21 |
-219 |
140 |
-20 |
15 |
815 |
447 |
|
SW22 |
428 |
670 |
1,390 |
|
240 |
-3255 |
|
Sample |
187Os/188Os |
187Re/188Os |
187Re/188Os |
87Rb/86Sr |
147Sm/144Nd |
176Lu/176Hf |
|
PL12 |
727 |
930 |
1,290 |
13 |
128 |
-1 |
|
PL13 |
-603 |
-280 |
-380 |
21 |
428 |
199 |
|
PL14 |
-389 |
-80 |
-120 |
4 |
1794 |
-1779 |
|
PL14 |
-21 |
260 |
320 |
|
|
|
|
PL15 |
623 |
840 |
1,100 |
5 |
232 |
-2614 |
|
PL16 |
-135 |
150 |
180 |
|
425 |
-143 |
|
PL16-R |
-130 |
160 |
-2,270 |
3 |
881 |
2285 |
|
PL16 |
-117 |
170 |
190 |
|
|
|
|
PL17 |
-124 |
160 |
220 |
|
847 |
2694 |
|
PL17 |
-48 |
230 |
310 |
|
|
|
|
PL18 |
1,230 |
1,390 |
-1,720 |
6 |
384 |
1740 |
|
PL18-R |
1,382 |
1,520 |
2,480 |
|
|
|
|
PL18 |
1,269 |
1,440 |
-380 |
|
|
|
|
PL19 |
-318 |
-10 |
-40 |
13 |
162 |
|
|
PL19 |
-27 |
250 |
380 |
|
14 |
1227 |
|
PL19-R |
-50 |
230 |
470 |
|
42 |
1345 |
|
PL23 |
798 |
990 |
1,130 |
5 |
1412 |
1308 |
|
PL23 |
719 |
920 |
1,040 |
|
967 |
1424 |
|
SW01 |
-1,366 |
-930 |
470 |
17 |
878 |
1895 |
|
SW02 |
-155 |
140 |
370 |
17 |
277 |
275 |
|
Sample |
187Os/188Os |
187Re/188Os |
187Re/188Os |
87Rb/86Sr |
147Sm/144Nd |
176Lu/176Hf |
|
MY9 |
2,397 |
2,600 |
4,050 |
|
|
|
|
MY9-R |
2,418 |
2,490 |
2,810 |
|
|
|
|
MY9 |
2,390 |
2,430 |
2,530 |
|
|
|
|
MY10 |
2,333 |
2,650 |
6,440 |
|
|
|
|
MY33 |
1,398 |
1,570 |
1,670 |
|
|
|
|
MY34 |
2,411 |
2,510 |
2,950 |
|
|
|
|
MY35 |
-1,111 |
-400 |
-2,680 |
|
|
|
|
PL01 |
-45 |
230 |
360 |
9 |
364 |
-244 |
|
PL02 |
888 |
1,080 |
1,340 |
8 |
347 |
-423 |
|
PL02 |
677 |
890 |
960 |
|
|
|
|
PL03 |
-263 |
40 |
70 |
|
408 |
-722 |
|
PL03-R |
-117 |
170 |
390 |
|
406 |
-865 |
|
PL03 |
-166 |
150 |
-30 |
|
|
|
|
PL06 |
-150 |
140 |
320 |
|
|
|
|
PL07 |
-296 |
20 |
|
|
|
|
|
PL07 |
-337 |
-30 |
-70 |
|
|
|
|
PL08 |
793 |
990 |
1,830 |
|
|
|
|
PL08 |
747 |
950 |
980 |
|
|
|
|
PL10 |
400 |
640 |
790 |
|
|
|
|
PL11 |
-4 |
270 |
360 |
6 |
601 |
1377 |
|
PL11 |
61 |
330 |
430 |
|
|
|
4. U-Th-Pb Systematics,
Geochimica et Cosmochimica Acta, 1981, Volume 45, Pages 635 - 645
|
Pb207/Pb206 |
Pb207/Pb206 |
|
4,747 |
3,899 |
|
4,739 |
3,802 |
|
4,549 |
3,666 |
|
4,548 |
3,664 |
|
4,316 |
3,575 |
|
4,315 |
3,572 |
|
4,207 |
3,256 |
|
4,205 |
3,214 |
|
4,165 |
3,212 |
|
4,164 |
3,194 |
|
4,141 |
3,028 |
|
3,933 |
2,596 |
|
3,918 |
2,583 |
|
3,917 |
2,568 |
5. Whole-Rock Pb/Pb Isotopic Ages,
Precambrian Research, Volume 78 (1996) 261-272
|
207Pb/206Pb |
207Pb/206Pb |
|
5,339 |
5,111 |
|
5,337 |
5,084 |
|
5,324 |
5,066 |
|
5,305 |
5,057 |
|
5,227 |
5,039 |
|
5,225 |
5,012 |
|
5,217 |
5,008 |
|
5,190 |
5,003 |
|
5,187 |
4,925 |
|
5,173 |
4,897 |
|
5,171 |
4,824 |
|
5,152 |
4,791 |
|
5,151 |
4,755 |
|
5,144 |
4,358 |
|
5,140 |
4,343 |
|
5,137 |
4,320 |
|
5,123 |
4,300 |
6. U-Pb Dating Of Madagascar,
Precambrian Research, 2003, Volume 121, Pages 73 - 84
|
206Pb/238U |
207Pb/235U |
207Pb/206Pb |
|
2,536 |
2,534 |
2,532 |
|
2,530 |
2,526 |
2,523 |
|
2,510 |
2,511 |
2,513 |
|
2,486 |
2,496 |
2,510 |
|
2,479 |
2,493 |
2,501 |
|
2,448 |
2,470 |
2,499 |
|
2,435 |
2,454 |
2,488 |
|
2,397 |
2,428 |
2,486 |
|
2,087 |
2,295 |
2,475 |
|
1,676 |
2,062 |
2,474 |
|
1,550 |
1,951 |
2,471 |
|
1,428 |
1,876 |
2,469 |
|
1,374 |
1,827 |
2,466 |
|
1,348 |
1,816 |
2,454 |
|
1,138 |
1,629 |
2,428 |
|
1,031 |
1,536 |
2,416 |
7. Pb Isotope Constraints,
Earth and Planetary Science Letters, Volume 142 (1996) 501-512
|
Pb207/Pb206 |
Pb207/Pb206 |
Pb207/Pb206 |
|
5,347 |
5,319 |
5,018 |
|
5,345 |
5,315 |
5,005 |
|
5,345 |
5,314 |
4,997 |
|
5,342 |
5,313 |
4,985 |
|
5,341 |
5,296 |
4,979 |
|
5,339 |
5,286 |
4,962 |
|
5,335 |
5,267 |
4,949 |
|
5,331 |
5,246 |
4,946 |
|
5,330 |
5,044 |
4,907 |
|
5,323 |
5,018 |
4,862 |
8. The Paleoproterozoic Huronian Supergroup,
Precambrian Research, Volume 102 (2000) 263–278
|
207Pb/206Pb |
207Pb/206Pb |
207Pb/206Pb |
|
5,012 |
4,625 |
4,304 |
|
4,918 |
4,592 |
4,287 |
|
4,877 |
4,536 |
4,084 |
|
4,871 |
4,531 |
3,992 |
|
4,784 |
4,505 |
3,856 |
|
4,777 |
4,452 |
3,770 |
|
4,751 |
4,445 |
3,753 |
|
4,716 |
4,442 |
3,559 |
|
4,635 |
4,413 |
3,028 |
|
4,628 |
4,327 |
|
9. Xenoliths from Yangyuan and Fansi,
Lithos, Volume 102, 2008, Pages 25-42
|
187Re/188Os |
187Re/188Os |
187Os/188Os |
|
-500 |
1,180 |
682 |
|
|
2,140 |
2,089 |
|
1,000 |
-530 |
-1,201 |
|
9,700 |
2,110 |
1,729 |
|
-200 |
|
|
|
2,600 |
1,710 |
1,271 |
|
-10,800 |
2,630 |
2,318 |
|
|
1,430 |
960 |
|
500 |
|
|
|
2,000 |
1,450 |
976 |
|
2,800 |
330 |
-268 |
|
-3,500 |
1,520 |
1,058 |
|
2,200 |
1,210 |
714 |
|
|
2,690 |
2,384 |
|
|
-310 |
-972 |
|
|
420 |
-170 |
|
|
1,680 |
1,238 |
|
|
1,720 |
1,287 |
|
|
1,420 |
943 |
10. Xenoliths from Kimberley, South Africa,
Geochimica et Cosmochimica Acta, 2008, Volume 72, Pages 5722-5756
|
187Re/188Os |
187Os/188Os |
187Re/188Os |
187Os/188Os |
187Re/188Os |
187Os/188Os |
|
3,250 |
3,218 |
2,690 |
2,416 |
3,020 |
2,940 |
|
1,560 |
1,123 |
2,740 |
2,547 |
2,810 |
2,678 |
|
-3,470 |
-4,850 |
2,690 |
2,531 |
3,050 |
2,956 |
|
2,610 |
2,384 |
2,640 |
2,449 |
2,740 |
2,547 |
|
2,600 |
2,384 |
3,190 |
2,809 |
3,050 |
2,940 |
|
-1,340 |
-8,206 |
1,540 |
927 |
2,590 |
2,318 |
|
3,140 |
-7,616 |
2,730 |
2,531 |
2,740 |
2,580 |
|
-600 |
-1,872 |
900 |
305 |
590 |
-104 |
|
-860 |
-1,839 |
2,240 |
1,893 |
-115,960 |
-62,462 |
|
2,810 |
2,678 |
2,390 |
2,155 |
-117,980 |
-62,118 |
|
187Re/188Os |
187Os/188Os |
187Re/188Os |
187Os/188Os |
187Re/188Os |
187Os/188Os |
|
3,930 |
3,218 |
-11,150 |
2,416 |
3,340 |
2,940 |
|
2,110 |
1,123 |
5,930 |
2,547 |
2,960 |
2,678 |
|
14,580 |
-4,850 |
2,810 |
2,531 |
4,350 |
2,956 |
|
5,200 |
2,384 |
3,580 |
2,449 |
5,020 |
2,547 |
|
4,870 |
2,384 |
-1,240 |
2,809 |
6,180 |
2,940 |
|
110 |
-8,206 |
-1,540 |
927 |
143,830 |
2,318 |
|
60 |
-7,616 |
6,600 |
2,531 |
3,270 |
2,580 |
|
290 |
-1,872 |
1,450 |
305 |
2,640 |
-104 |
|
-15,020 |
-1,839 |
21,670 |
1,893 |
7,050 |
-62,462 |
|
3,050 |
2,678 |
2,850 |
2,155 |
90,440 |
-62,118 |
11. Re-Os Isotopic Evidence From Mantle Xenoliths,
Contributions Mineral Petrology, 2008, Volume 155, Pages 271-293
|
87Rb/86Sr |
147Sm/144Nd |
187Re/188Os |
|
141 |
141 |
327 |
|
141 |
141 |
141 |
|
141 |
141 |
141 |
|
141 |
141 |
141 |
|
465 |
465 |
140 |
|
465 |
466 |
467 |
|
464 |
465 |
466 |
|
465 |
465 |
465 |
|
454 |
465 |
477 |
|
466 |
465 |
463 |
|
465 |
465 |
467 |
|
465 |
466 |
474 |
|
465 |
466 |
464 |
|
2,135 |
489 |
465 |
|
1,383 |
445 |
465 |
|
465 |
465 |
471 |
|
120 |
120 |
465 |
|
120 |
120 |
465 |
|
127 |
120 |
467 |
12. Timing of Precambrian Melt Depletion,
Lithos, Volume 77, 2004, Pages 453-472
|
Sample |
187Re/188Os |
187Re/188Os |
206Pb/204Pb |
147Sm/144Nd |
176Lu/176Hf |
187Os/188Os |
|
13-16-3 |
2,530 |
3,030 |
|
1,130 |
1,030 |
1,472 |
|
13-19-11 |
2,650 |
6,000 |
4,840 |
1,280 |
1,310 |
73 |
|
13-19-15 |
2,770 |
7,460 |
4,879 |
1,290 |
1,320 |
-242 |
|
13-19-2 |
2,610 |
3,470 |
4,881 |
1,230 |
1,260 |
-1,187,221 |
|
13-19-22 |
|
47,370 |
4,857 |
1,380 |
1,400 |
945 |
|
13-19-27 |
|
49,630 |
5,118 |
1,430 |
1,500 |
-395 |
|
13-19-6 |
2,620 |
4,540 |
5,103 |
1,280 |
1,300 |
2,015 |
|
HK1-13H |
740 |
-1,240 |
5,018 |
-2,340 |
-4,240 |
2,421 |
|
HK1-13W |
910 |
-1,240 |
5,025 |
-1,750 |
-1,470 |
2,006 |
|
HK1-19 |
1,140 |
-220 |
4,421 |
-980 |
-1,140 |
2,446 |
|
HK1-21 |
1,560 |
830 |
5,022 |
|
|
2,166 |
|
HK1-24 |
1,570 |
2,000 |
4,986 |
-180 |
40 |
1,140 |
|
HK1-25/2 |
1,900 |
2,280 |
5,029 |
650 |
580 |
2,605 |
|
HK1-26 |
2,300 |
2,670 |
4,916 |
770 |
630 |
2,199 |
|
HK-3aa |
2,450 |
2,930 |
5,022 |
1,020 |
1,030 |
-8,589 |
|
HK4-1 |
2,420 |
2,870 |
5,001 |
920 |
870 |
2,482 |
13. Reliable Re-Os Ages,
Geochimica et Cosmochimica Acta, 1993, Volume 57, Page 1626
|
187Re/188Os |
|
5,930 |
|
6,300 |
|
1,710 |
14. Re-Os, Sm-Nd, and Rb-Sr Isotope Evidence,
Geochemica et Cosmochimica Acta, 1995, Volume 59, Number 5, Pages 959-977
|
187Os/188Os |
187Os/188Os |
|
-1,584,771 |
488 |
|
-1,503,264 |
672 |
|
-477,884 |
847 |
|
-34,888 |
891 |
|
-19,080 |
1,277 |
|
-6,469 |
1,331 |
|
-1,548 |
1,739 |
|
-721 |
2,169 |
|
192 |
2,230 |
|
254 |
2,402 |
|
263 |
2,785 |
|
269 |
2,790 |
|
330 |
|
|
187Re/188Os |
187Re/188Os |
147Sm/144Nd |
147Sm/144Nd |
87Rb/86Sr |
|
5,500 |
2,600 |
|
|
|
|
Negative |
1,800 |
|
|
|
|
Negative |
1,900 |
1,900 |
2,300 |
|
|
2,500 |
2,000 |
1,700 |
2,100 |
8,300 |
|
400 |
400 |
|
|
|
|
500 |
|
|
|
|
|
Negative |
2,100 |
|
|
|
|
11,000 |
1,000 |
|
|
|
|
2,200 |
1,700 |
|
|
|
|
Negative |
1,800 |
Negative |
Negative |
Negative |
|
Negative |
3,200 |
2,700 |
2,900 |
Negative |
|
3,100 |
2,900 |
|
|
|
|
3,000 |
1,800 |
|
|
|
|
|
|
2,000 |
2,300 |
990 |
|
|
|
2,100 |
2,500 |
Negative |
|
4,100 |
3,000 |
3,000 |
3,200 |
Negative |
|
6,900 |
2,800 |
Negative |
Negative |
Negative |
|
|
|
1,800 |
2,200 |
|
|
|
|
2,300 |
2,500 |
|
|
6,600 |
1,500 |
|
|
|
|
100 |
1,200 |
|
|
|
|
Negative |
1,100 |
|
|
|
|
2,700 |
|
|
|
|
|
3,100 |
|
3,000 |
|
|
15. Lithospheric Mantle and Diamonds,
Lithos, Volume 112-S, 2009, Pages 1120-1132
|
187Re/188Os |
187Re/188Os |
|
7,850 |
2,840 |
|
6,260 |
2,760 |
|
4,210 |
2,730 |
|
4,180 |
2,690 |
|
4,040 |
2,660 |
|
3,850 |
2,660 |
|
3,470 |
2,580 |
|
3,310 |
2,580 |
|
3,280 |
2,560 |
|
3,250 |
2,490 |
|
3,120 |
2,130 |
|
2,980 |
1,980 |
|
2,960 |
1,980 |
16. Pb-Pb Isotope Systematics,
Chemical Geology, Volume 66 (1987) Pages 193-208
|
207Pb/206Pb |
207Pb/206Pb |
207Pb/206Pb |
|
5,289 |
5,036 |
4,447 |
|
5,289 |
5,030 |
4,410 |
|
5,267 |
5,030 |
4,408 |
|
5,259 |
5,021 |
4,168 |
|
5,259 |
5,013 |
4,102 |
|
5,256 |
5,001 |
4,096 |
|
5,243 |
5,001 |
4,082 |
|
5,240 |
4,998 |
4,077 |
|
5,240 |
4,998 |
4,073 |
|
5,210 |
4,925 |
4,051 |
|
5,210 |
4,925 |
4,030 |
|
5,200 |
4,756 |
4,026 |
|
5,200 |
4,749 |
3,992 |
|
5,153 |
4,704 |
3,968 |
|
5,153 |
4,667 |
3,956 |
|
5,151 |
4,625 |
3,917 |
|
5,151 |
4,622 |
3,908 |
|
5,148 |
4,618 |
3,883 |
|
5,148 |
4,615 |
3,870 |
|
5,103 |
4,604 |
3,829 |
|
5,103 |
4,531 |
3,811 |
|
5,099 |
4,468 |
3,728 |
|
5,060 |
4,466 |
3,719 |
|
5,036 |
4,447 |
|
17. Sm-Nd, Rb-Sr, And Pb-Pb Isotopic Evidence,
Gondwana Research, Volume 11 (2007) Page 69-91
|
207Pb/206Pb |
207Pb/206Pb |
|
5,333 |
5,084 |
|
5,327 |
5,084 |
|
5,326 |
5,080 |
|
5,304 |
5,076 |
|
5,303 |
5,076 |
|
5,253 |
5,073 |
|
5,224 |
5,072 |
|
5,205 |
5,066 |
|
5,205 |
5,060 |
|
5,183 |
5,050 |
|
5,180 |
5,043 |
|
5,161 |
5,034 |
|
5,130 |
5,032 |
|
5,116 |
5,031 |
|
5,096 |
5,022 |
|
5,092 |
5,018 |
|
5,091 |
|
18. Pb and Nd Isotope Systematics,
Precambrian Research, Volume 114 (2002) 277-294
|
207Pb/206Pb |
207Pb/206Pb |
207Pb/206Pb |
207Pb/206Pb |
|
5,319 |
5,189 |
5,073 |
4,994 |
|
5,301 |
5,189 |
5,069 |
4,984 |
|
5,291 |
5,133 |
5,060 |
4,977 |
|
5,288 |
5,128 |
5,050 |
4,968 |
|
5,286 |
5,115 |
5,047 |
4,961 |
|
5,281 |
5,102 |
5,044 |
4,947 |
|
5,268 |
5,096 |
5,043 |
4,945 |
|
5,249 |
5,089 |
5,022 |
4,938 |
|
5,236 |
5,082 |
5,022 |
4,913 |
|
5,206 |
5,081 |
5,009 |
4,873 |
|
5,196 |
5,080 |
4,995 |
|
19. Crustal Age Domains,
Journal Of Petrology, 1998, Volume 39, Number 4, Pages 749-783
|
207Pb/206Pb |
207Pb/206Pb |
207Pb/206Pb |
|
5,333 |
5,161 |
5,073 |
|
5,327 |
5,130 |
5,072 |
|
5,326 |
5,116 |
5,066 |
|
5,304 |
5,096 |
5,060 |
|
5,303 |
5,092 |
5,050 |
|
5,253 |
5,091 |
5,043 |
|
5,224 |
5,084 |
5,034 |
|
5,205 |
5,084 |
5,032 |
|
5,205 |
5,080 |
5,031 |
|
5,183 |
5,076 |
5,022 |
|
5,180 |
5,076 |
5,018 |
20. The Slave Craton, Canada,
Geochimica et Cosmochimica Acta, Volume 74 (2010) Pages 5368-5381
|
187Re/188Os |
187Os/188Os |
|
2,140 |
-830,588 |
|
2,550 |
-617,820 |
|
1,760 |
-814,222 |
|
2,160 |
-1,157,924 |
|
432 |
-28,615 |
|
2,960 |
-61,349 |
|
3,160 |
-3,220,142 |
|
3,900 |
-4,103,949 |
|
2,600 |
-994,256 |
|
3,800 |
-61,349 |
|
3,570 |
-159,549 |
|
4,530 |
-2,712,771 |
|
5,800 |
-683,287 |
|
5,800 |
-1,714,396 |
|
2,340 |
-2,810,972 |
|
3,500 |
-945,156 |
|
3,400 |
-1,059,724 |
|
1,240 |
-1,337,959 |
|
2,110 |
-1,174,291 |
|
2,660 |
-1,812,597 |
|
2,510 |
-1,190,658 |
|
2,360 |
-896,056 |
|
2,850 |
-1,043,357 |
21. The Study of Molybdenites,
Earth and Planetary Science Letters, 1982, Volume 61, Page 293
|
Location |
Country |
Re/Os Age |
Model Age |
Model Age |
Model Age |
|
Ylitornio |
(Lapland) |
1,770 |
1,780 |
|
|
|
Tepasto |
(Lapland) |
1,590 |
1,800 |
|
|
|
|
|
4,490 |
|
|
|
|
Lahnanen |
(Finland) |
1,880 |
1,890 |
|
|
|
Matasvaara |
(Finland) |
1,840 |
2,700 |
2,400 |
176 |
|
Biggenden |
(Australia) |
330 |
215 |
|
|
|
Mt. Mulgine |
(Australia) |
2,670 |
2,690 |
|
|
|
Everton |
(Australia) |
376 |
377 |
|
|
|
Mt. Moliagul |
(Australia) |
920 |
276 |
390 |
|
|
Climax |
(Colorado, U.S.A.) |
96 |
30 |
|
|
|
Montezuma |
(Mexico) |
|
60 |
|
|
|
Godthaab |
(Greenland) |
1,840 |
2,000 |
1,600 |
2,700 |
|
Lacorne Preissac |
(Quebec, Canada) |
6,370 |
2,700 |
|
|
|
|
|
|
|
6,800 |
2,700 |
22. North Western Wyoming Craton,
Earth And Planetary Science Letters, 1994, Volume 126, Page 460
|
207Pb/206Pb |
87Rb/86Sr |
|
5,398 |
1,750 |
|
5,407 |
1,910 |
|
5,435 |
1,470 |
|
5,541 |
4,040 |
|
5,499 |
3,440 |
|
5,458 |
520 |
|
5,454 |
150 |
|
5,442 |
120 |
|
5,752 |
10,800 |
|
5,422 |
3,180 |
|
5,457 |
15,500 |
|
5,482 |
-3,440 |
|
5,436 |
2,140 |
|
5,567 |
4,440 |
|
5,570 |
|
|
5,428 |
240 |
|
5,467 |
170 |
|
5,466 |
120 |
|
87Rb/86Sr |
147Sm/144Nd |
207Pb/206Pb |
|
5,170 |
3,460 |
4,770 |
|
-630 |
2,550 |
5,195 |
|
-930 |
2,490 |
5,145 |
|
2,600 |
2,500 |
5,121 |
|
110 |
2,610 |
5,108 |
|
-300 |
2,630 |
5,137 |
|
|
2,510 |
1,776 |
|
|
2,540 |
1,763 |
|
187Os/188Os |
187Re/1880s |
187Re/1880s |
|
-2,665 |
|
1,310 |
|
-33,561 |
|
2,750 |
|
-30,751 |
|
3,320 |
|
-25,270 |
|
2,780 |
|
-15,464 |
|
560 |
|
-2,409 |
|
530 |
|
1,688 |
2,040 |
|
|
1,680 |
1,960 |
|
|
2,575 |
2,900 |
|
|
-980 |
660 |
80 |
|
1,320 |
1,730 |
|
|
-17 |
430 |
680 |
|
2,382 |
2,680 |
|
|
2,511 |
2,880 |
|
|
1,186 |
1,580 |
|
|
881 |
1,460 |
|
|
-39,504 |
|
1,420 |
|
-5,868 |
|
1,920 |
23. Re-Os, and Mo Isotope Systematics,
Geochimica et Cosmochimica Acta, Volume 69, Number 7, Pages 1787–1801, 2005
|
187Os/188Os |
187Os/188Os |
|
-2,409,985 |
-62,920 |
|
-1,453,836 |
-60,285 |
|
-488,031 |
-49,172 |
|
-319,453 |
-47,421 |
|
-249,403 |
-40,792 |
|
-177,651 |
-40,072 |
|
-163,969 |
-39,253 |
|
-108,223 |
-36,242 |
|
-100,318 |
-36,013 |
|
-87,225 |
-29,924 |
|
-82,036 |
-26,389 |
|
-80,481 |
-25,456 |
|
-79,270 |
-23,132 |
|
-70,285 |
|
24. Re-Os Systematics of Komatiites,
Geochimica et Cosmochimica Acta, Volume 69, Number 21, Pages 5087–5098, 2005
|
187Os/188Os |
187Os/188Os |
|
-82,331 |
-16,242 |
|
-52,723 |
-15,669 |
|
-51,169 |
-3,099 |
|
-40,465 |
-890 |
|
-33,689 |
27 |
|
-32,281 |
338 |
|
-30,677 |
878 |
|
-22,461 |
1,320 |
|
-20,694 |
1,353 |
|
-19,875 |
1,533 |
|
-18,697 |
1,565 |
|
-18,517 |
1,582 |
|
-17,076 |
|
25. Belingwe and Abitibi Komatiites,
Geochimica et Cosmochimica Acta, Volume 73 (2009) 6367–6389
|
187Os/188Os |
187Os/188Os |
187Os/188Os |
187Os/188Os |
|
-74,385 |
-4,613 |
-2,633 |
-613 |
|
-58,661 |
-3,864 |
-2,546 |
911 |
|
-40,466 |
-3,778 |
-2,099 |
925 |
|
-32,149 |
-3,675 |
-2,071 |
1,087 |
|
-8,600 |
-3,296 |
-1,954 |
1,357 |
|
-7,559 |
-3,222 |
-1,451 |
1,380 |
|
-5,983 |
-2,844 |
-1,400 |
1,457 |
|
-5,274 |
-2,810 |
-1,284 |
1,726 |
|
-4,646 |
-2,805 |
-1,071 |
2,646 |
|
-4,618 |
-2,667 |
-996 |
|
26. Mantle Xenoliths From Namibia,
Lithos, Volume 184–187 (2014) 478–490
|
187Os/188Os |
187Os/188Os |
187Os/188Os |
187Os/188Os |
187Os/188Os |
|
-44,982 |
-4,114 |
-305 |
1,091 |
2,089 |
|
-44,982 |
-4,048 |
-291 |
1,189 |
2,089 |
|
-43,345 |
-2,975 |
-286 |
1,205 |
2,105 |
|
-34,900 |
-2,975 |
-268 |
1,320 |
2,204 |
|
-34,900 |
-2,958 |
-232 |
1,353 |
2,220 |
|
-34,622 |
-448 |
-232 |
1,353 |
2,220 |
|
-34,556 |
-443 |
-194 |
1,369 |
2,236 |
|
-34,474 |
-443 |
-192 |
1,385 |
2,253 |
|
-34,474 |
-431 |
-153 |
1,402 |
2,253 |
|
-28,615 |
-422 |
-153 |
1,418 |
2,253 |
|
-12,248 |
-422 |
-153 |
1,434 |
2,515 |
|
-12,248 |
-376 |
-153 |
1,434 |
2,515 |
|
-9,458 |
-361 |
-153 |
1,434 |
2,951 |
|
-8,909 |
-353 |
583 |
1,729 |
20,011 |
|
-8,828 |
-337 |
583 |
1,778 |
20,358 |
|
-8,615 |
-333 |
894 |
1,909 |
20,376 |
|
-8,533 |
-317 |
976 |
1,942 |
20,425 |
|
-5,702 |
-314 |
976 |
1,991 |
20,435 |
|
-4,801 |
-309 |
992 |
2,024 |
20,469 |
|
-4,736 |
-307 |
1,074 |
2,040 |
20,469 |
27. 187Os Isotopic Constraints,
Geochimica et Cosmochimica Acta, 2002, Volume 66, Number 18, Pages 3317-3325
|
187Os/188Os |
187Os/188Os |
|
-456,934 |
-12,782 |
|
-308,455 |
-8,638 |
|
-83,799 |
-8,073 |
|
-73,472 |
-6,531 |
|
-67,167 |
-6,255 |
|
-51,642 |
1,446 |
|
-50,817 |
1,672 |
|
-36,489 |
1,834 |
|
-24,396 |
2,112 |
|
-23,900 |
2,300 |
|
-21,491 |
2,372 |
|
-13,877 |
|
28. Evidence from 2.8 Ga Komatiites,
Earth and Planetary Science Letters, 2001, Volume 186, Pages 513-526
|
187Os/188Os |
187Os/188Os |
|
-19,486 |
-8,384 |
|
-17,888 |
-3,309 |
|
-16,094 |
-1,782 |
|
-14,527 |
-882 |
|
-14,510 |
-602 |
|
-12,098 |
-34 |
|
-9,284 |
2,215 |
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Pages 1857-1898
2. Diamonds And Mantle-Derived Xenoliths, Earth and Planetary Science Letters, Volume 42, 1979, Pages 58-70
3. Temporal Evolution of the Lithospheric Mantle, Journal Of Petrology, 2009, Volume 50, Number 10,
Pages 1857-1898
4. U-Th-Pb Systematics, Geochimica et Cosmochimica Acta, Volume 45. pp. 635 to 645, 1981
5. Whole-Rock Pb/Pb Isotopic Ages, Precambrian Research, Volume 78 (1996) 261-272
6. U-Pb dating Of Madagascar, Precambrian Research, 2003, Volume 121, Pages 73 - 84
7. Pb Isotope Constraints, Earth and Planetary Science Letters, Volume 142 (1996) 501-512
8. The Paleoproterozoic Huronian Supergroup, Precambrian Research, Volume 102 (2000) 263–278
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10. Xenoliths from Kimberley, South Africa, Geochimica et Cosmochimica Acta, 2008, Volume 72,
Pages 5722-5756
11. Re-Os Isotopic Evidence From Mantle Xenoliths, Contributions Mineral Petrology, 2008, Volume 155,
Pages 271-293
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13. Reliable Re-Os Ages, Geochimica et Cosmochimica Acta, 1993, Volume 57, Page 1626
14. Re-Os, Sm-Nd, and Rb-Sr Isotope Evidence, Geochemica et Cosmochimica Acta, 1995, Volume 59,
Number 5, Pages 959-977
15. Lithospheric Mantle and Diamonds, Lithos, Volume 112-S, 2009, Pages 1120-1132
16. Pb-Pb Isotope Systematics, Chemical Geology, Volume 66 (1987) Pages 193-208
17. Sm-Nd, Rb-Sr, And Pb-Pb Isotopic Evidence, Gondwana Research, Volume 11 (2007) Page 69-91
18. Pb and Nd Isotope Systematics, Precambrian Research, Volume 114 (2002) 277-294
19. Crustal Age Domains, Journal Of Petrology, 1998, Volume 39, Number 4, Pages 749-783
20. The Slave Craton, Canada, Geochimica et Cosmochimica Acta, Volume 74 (2010) Pages 5368-5381
21. The Study of Molybdenites, Earth and Planetary Science Letters, 1982, Volume 61, Page 293
22. North Western Wyoming Craton, Earth And Planetary Science Letters, 1994, Volume 126, Page 460
23. Re-Os, and Mo isotope systematics, Geochimica et Cosmochimica Acta, Volume 69, Number 7,
Pages 1787–1801, 2005
24. Re-Os systematics of komatiites, Geochimica et Cosmochimica Acta, Volume 69, Number 21,
Pages 5087–5098, 2005
25. Belingwe and Abitibi komatiites, Geochimica et Cosmochimica Acta, Volume 73 (2009) 6367–6389
26. Mantle Xenoliths from Namibia, Lithos, Volume 184–187 (2014) 478–490
27. 187Os isotopic constraints, Geochimica et Cosmochimica Acta, 2002, Volume 66, Number 18, Pages 3317-3325
28. Evidence from 2.8 Ga Komatiites, Earth and Planetary Science Letters, 2001, Volume 186, Pages 513-526