Why subduction zones are curved
Author:
Affiliation:
1. School of Engineering and Applied Sciences; Harvard University; Cambridge; Massachusetts; USA
2. Department of Geosciences; University of Montana; Missoula; Montana; USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://www.agu.org/journals/tc/tc1006/2010TC002720/2010TC002720.pdf
Reference42 articles.
1. The curvature of Wadati-Benioff zones and the torsional rigidity of subducting plates;Bevis;Nature,1986
2. Newtonian versus non-Newtonian upper mantle viscosity: Implications for subduction initiation;Billen;Geophys. Res. Lett.,2005
3. Multiscale dynamics of the Tonga-Kermadec subduction zone;Billen;Geophys. J. Int.,2003
4. Subduction of oceanic plateaus, continental margins, island arcs, spreading ridges, and seamounts;Cloos;Geol. Soc. Am. Bull.,1993
5. The temporal evolution of plate driving forces: Importance of “slab suction” versus “slab pull” during the Cenozoic;Conrad;J. Geophys. Res.,2004
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