Where the Pacific and Australian tectonic plates collide under the South Island of New Zealand large quantities of aqueous fluid are produced. But how does this happen? Geophysical and petrological data indicate that it may not be as we thought.
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 12 print issues and online access
$259.00 per year
only $21.58 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
Vry, J., Powell, R., Golden, K. & Petersen, K. Nature Geosci. 3, 31–35 (2010).
Miyashiro, A. Metamorphic Petrology (Oxford Univ. Press, 1994).
Cox, S. & Sutherland, R. in A Continental Boundary: Tectonics at South Island, New Zealand (eds Okaya, D., Stern, T. & Davey, F.) 19–46 (Geophysical Monograph Series Vol. 175, American Geophysical Union, 2007).
Stern, T. et al. in A Continental Boundary: Tectonics at South Island, New Zealand (eds Okaya, D., Stern, T. & Davey, F.) 209–236 (Geophysical Monograph Series Vol. 175, American Geophysical Union, 2007).
Wannamaker, P. et al. J. Geophys. Res. 107, 2117 (2002).
Jiracek, G. et al. in A Continental Boundary: Tectonics at South Island, New Zealand (eds Okaya, D., Stern, T. & Davey, F.) 75–94 (Geophysical Monograph Series Vol. 175, American Geophysical Union, 2007).
Wannamaker, P. et al. Nature 460, 733–736 (2009).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Wannamaker, P. Water from stone. Nature Geosci 3, 10–11 (2010). https://doi.org/10.1038/ngeo732
Issue Date:
DOI: https://doi.org/10.1038/ngeo732