Nature Publishing Group, publisher of Nature, and other science journals and reference works
my account e-alerts subscribe register
Tuesday 25 July 2017
Journal Home
Current Issue
Download PDF
Export citation
Export references
Send to a friend
More articles like this

Letters to Nature
Nature 321, 766 - 769 (19 June 1986); doi:10.1038/321766a0

Jack Hills, evidence of more very old detrital zircons in Western Australia

W. Compston* & R. T. Pidgeon

*Research School of Earth Sciences, The Australian National University, GPO Box 4, Canberra, A.C.T. 2600, Australia
Department of Physics and Geoscience, Western Australian Institute of Technology, Bentley, Western Australia 6102, Australia

The age of the Earth's oldest crustal minerals sets a time-limit on the earliest preservation of buoyant solid crust. The oldest mineral ages reported so far are ~4,180 Myr for detrital zircons from quartzites at Mount Narryer1, in the Yilgarn Block, Western Australia. The oldest-known intact rocks, as distinct from individual minerals, are substantially younger; they formed ~3,813-Myr ago2 in the Isua supracrustal belt, West Greenland. We report here a further occurrence of old detrital zircons, again identified using the ion-microprobe SHRIMP3, in conglomerate from the Jack Hills Metasedimentary Belt4,5 (26°11′ S, 116°58′ E), ~60km north-east of Narryer. This discovery is important for several reasons. First, one zircon registers the exceptionally old age of 4,276±6 Myr, which is, moreover, a minimum estimate for its original age; 16 other grains may have the same age or may be slightly younger. Second, the new occurrence considerably extends the area over which the old Narryer suite is known, thus amplifying its geological significance. Third, the frequency of old zircons in the Jack Hills occurrence is 12%, about five times higher than at Narryer, which suggests that the intact ~4,180 Myr-old rocks, if they still exist, might be closer, and facilitates future comparison of the SHRIMP data with conventional analyses of these grains. (Recent conventional U–Pb work6 on other zircons from the same Narryer concentrate confirmed the younger ages but failed to observe any at ~4,180 Myr, probably because of their low abundance7). The likelihood that zircon would dissolve in magmas undersaturated in zirconium8 argues against its survival in long-term contact with such magmas during the disaggregation and subduction of crust. Consequently, the existence of zircon in the Jack Hills area from ~4,300 Myr ago implies that this part of the crust has been preserved, since then, from recirculation in the mantle through plate-tectonics or any other mechanism.



1. Froude, D. O. et al. Nature 304, 616−618 (1983). | ISI | ChemPort |
2. Baadsgaard, H. et al. Earth planet. Sci. Lett. 68, 221−228 (1984). | Article | ISI | ChemPort |
3. Compston, W., Williams, I. S. & Meyer, C. J. geophys. Res. 89, B525−534 (1984). | ChemPort |
4. Elias, M. Geol. Surv. Western Australia Belele Explan. Not. (1983).
5. Baxter, J. L., Wilde, S. A., Pidgeon, R. T. & Fletcher, I. R. 7th Australian Geol. Conv. 56−57 (1984).
6. Scharer, U. & Allègre, C. Nature 315, 52−55 (1985). | ISI |
7. Compston, W. et al. Nature 317, 559−560 (1985). | PubMed | ISI | ChemPort |
8. Watson, E. B. & Harrison, T. M. Earth planet. Sci. Lett. 64, 295−304 (1983). | Article | ISI | ChemPort |
9. Williams, I. R., Walker, I. M., Hocking, R. M. & Williams, S. J. Geol. Surv. Western Australia Rec. 5 (1980).
10. Williams, I. S., Compston, W., Black, L. P., Ireland, T. R. & Foster, J. J. Contr. Miner. Petrol. 88, 322−327 (1984). | ISI | ChemPort |
11. Compston, W., Williams, I. S. & McCulloch, M. T. Aust. J. Earth Sci. (in the press).
12. Pidgeon, R. T. & Bowes, D. R. Geol. Mag. 109, 247−258 (1972). | ISI | ChemPort |

© 1986 Nature Publishing Group
Privacy Policy