Low heat flow inferred from >4 Gyr zircons suggests Hadean plate boundary interactions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/nature07465.pdf
Reference32 articles.
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2. Mojzsis, S. J., Harrison, T. M. & Pidgeon, R. T. Oxygen-isotope evidence from ancient zircons for liquid water at the Earth's surface 4,300 Myr ago. Nature 409, 178–181 (2001)
3. Cavosie, A. J., Valley, J. W. & Wilde, S. A. Magmatic δ18O in 4400–3900 Ma detrital zircons: a record of the alteration and recycling of crust in the Early Archean. Earth Planet. Sci. Lett. 235, 663–681 (2005)
4. Trail, D. et al. Constraints on Hadean zircon protoliths from oxygen isotopes, REEs and Ti-thermometry. Geochem. Geophys. Geosyst. 8, Q06014 10.1029/2006GC001449 (2007)
5. Turner, G., Harrison, T. M., Holland, G., Mojzsis, S. J. & Gilmour, J. Extinct Pu-244 in ancient zircons. Science 306, 89–91 (2004)
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