The influence of the region where the lower mantle meets the core extends to Earth's surface. A computational study of mineral properties shows one way forward in understanding this enigmatic zone.
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 Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
References
Ammann, M. W., Brodholt, J. P., Wookey, J. & Dobson, D. P. Nature 465, 462–465 (2010).
Lay, T., Williams, Q. & Garnero, E. J. Nature 392, 461–468 (1998).
Karato, S. & Weidner, D. J. Elements 4, 191–196 (2008).
Murakami, M., Hirose, K., Kawamura, K., Sata, N. & Ohishi, Y. Science 304, 855–858 (2004).
Wentzcovitch, R. & Stixrude, L. (eds) Rev. Miner. Geochem. 71 (2010).
Mitrovica, J. X. & Forte, A. M. Earth Planet. Sci. Lett. 225, 177–189 (2004).
Catalli, K., Shim, S.-H. & Prakapenka, V. Nature 462, 782–785 (2009).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Van Orman, J. Our planet's internal weakness. Nature 465, 432–433 (2010). https://doi.org/10.1038/465432a
Published:
Issue Date:
DOI: https://doi.org/10.1038/465432a