Simulations of Earth's growth show a correlation between the timing of the Moon's formation and the amount of mass that Earth accreted afterwards. This relationship provides a way of measuring the age of our planet. See Letter p.84
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on SpringerLink
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Amelin, Y. et al. Earth Planet. Sci. Lett. 300, 343–350 (2010).
Connelly, J. N. et al. Science 338, 651–655 (2012).
Yin, Q. et al. Nature 418, 949–952 (2002).
Allègre, C. J., Manhès, G. & Göpel, C. Earth Planet. Sci. Lett. 267, 386–398 (2008).
Halliday, A. N. Phil. Trans. R. Soc. A 366, 4163–4181 (2008).
Jacobson, S. A. et al. Nature 508, 84–87 (2014).
Canup, R. M. & Asphaug, E. Nature 412, 708–712 (2001).
Morbidelli, A., Lunine, J. I., O'Brien, D. P., Raymond, S. N. & Walsh, K. J. Annu. Rev. Earth Planet. Sci. 40, 251–275 (2012).
Walker, R. J. Chem. Erde Geochem. 69, 101–125 (2009).
Valley, J. W. et al. Nature Geosci. 7, 219–223 (2014).
Dong, S. & Zhu, Z. Astrophys. J. 778, 53 (2013).
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Chambers, J. A chronometer for Earth's age. Nature 508, 51–52 (2014). https://doi.org/10.1038/508051a
Published:
Issue Date:
DOI: https://doi.org/10.1038/508051a