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Controls on trench topography from dynamic models of subducted slabs

Zhong, Shijie and Gurnis, Michael (1994) Controls on trench topography from dynamic models of subducted slabs. Journal of Geophysical Research B, 99 (B8). pp. 15683-15695. ISSN 0148-0227. http://resolver.caltech.edu/CaltechAUTHORS:20130507-104326549

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Abstract

A finite element method with constrained elements and Lagrange multipliers is used to study tectonic faults in a viscous medium. A fault, representing the interface between overriding and subducting plates, has been incorporated into a viscous flow model of a subduction zone in which both thermal buoyancy and the buoyancy associated with the phase change from olivine to spinel are included. The fault causes stress to concentrate in its vicinity, giving rise to a weak plate margin and a mobile plate if a power law rheology is used. Surface dynamic topography with either a Newtonian or a power law rheology and with typical subduction zone parameters is characterized by a narrow and deep trench and a broadly depressed back arc basin. This suggests that oceanic trenches and back arc basins over subduction zones are dynamically compensated by viscous flow. Our models show that trench depth increases with fault dip angle, slab dip angle, slab length, and age of oceanic lithosphere just prior to subduction. The influence of fault dip angle and age of lithosphere on trench depth is greater than the influence of slab dip angle and slab length. These relationships of trench depth versus subduction zone parameters explain well the statistics of observed trench depths. For those subduction zones with oceanic lithosphere on both sides of the trench, observed trench depths have been corrected for fault and slab dip angles, based on the relationships from the dynamic models. After correction to a common set of parameters, trench depth correlates linearly with age of lithosphere prior to subduction with a slope which is close to what models having high viscosities within the transition zone and lower mantle predict. Comparison between the trench depths, corrected for fault and slab dip angles, and model trench depths suggests that the resisting tangential stress on faults in subduction zones may range from 15 MPa to 30 MPa, depending on model details.


Item Type:Article
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http://dx.doi.org/10.1029/94JB00809DOIUNSPECIFIED
http://onlinelibrary.wiley.com/doi/10.1029/94JB00809/abstractPublisherUNSPECIFIED
Additional Information:© 1994 by the American Geophysical Union. Received June 14, 1993; revised March 10, 1994; accepted March 21, 1994. We thank L. Ruff and G. Houseman for constructive discussions and M. Parmentier, S. Willen, and the Associate Editor for their reviews. This work was funded by the David and Lucile Packard Foundation and NSF grant EAR-8957164. Contribution number 5414, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California.
Group:Seismological Laboratory
Funders:
Funding AgencyGrant Number
David and Lucile Packard FoundationUNSPECIFIED
NSFEAR-8957164
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Caltech Division of Geological and Planetary Sciences5414
Record Number:CaltechAUTHORS:20130507-104326549
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20130507-104326549
Official Citation:Zhong, S., and M. Gurnis (1994), Controls on trench topography from dynamic models of subducted slabs, J. Geophys. Res., 99(B8), 15683–15695, doi:10.1029/94JB00809.
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:38322
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:07 May 2013 17:58
Last Modified:11 Jun 2015 12:59

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