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Role of faults, nonlinear rheology, and viscosity structure in generating plates from instantaneous mantle flow models

Zhong, Shijie and Gurnis, Michael and Moresi, Louis (1998) Role of faults, nonlinear rheology, and viscosity structure in generating plates from instantaneous mantle flow models. Journal of Geophysical Research B, 103 (B7). pp. 15255-15268. ISSN 0148-0227. http://resolver.caltech.edu/CaltechAUTHORS:20130123-074905905

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Abstract

Concentrated strain within plate margins and a significant toroidal component in global plate motion are among the most fundamental features of plate tectonics. A significant proportion of strain in plate margins is accommodated through motion on major tectonic faults. The decoupling influence of faulted plate margins primarily results from history-dependent lithospheric deformation rather than from instantaneous stress-weakening rheologies. For instantaneous mantle flow models, we argue that faults should be treated as preexisting mechanical structures. With models incorporating preexisting faults, a power law rheology with an exponent of 3, and slab pull and ridge push forces, we demonstrate that nonlinear interaction between weak faults and this power law rheology produces plate-like motion. Our models show that in order to produce plate-like motion, the frictional stress on faults needs to be small and the asthenosphere viscosity should be much weaker than that of lithosphere. While both plateness and the ratio of toroidal to poloidal velocities are reduced with increasing fault coupling, the viscosity contrast between the lithosphere and asthenosphere only influences plateness. This shows that both diagnostics, plateness and the ratio of toroidal to poloidal velocities, are necessary to characterize plate motion. The models demonstrate that weak transform faults can guide plate motion. This guiding property of transform faults and the decoupling of thrust faults result in oblique subduction where the strike of subducted slabs is oblique to transform faults. Subducted slabs beneath a dipping fault produce oceanic trench and fore bulge topography and principal stresses consistent with subduction zone observations.


Item Type:Article
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URLURL TypeDescription
http://dx.doi.org/10.1029/98JB00605 DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/98JB00605/abstractPublisherArticle
ORCID:
AuthorORCID
Gurnis, Michael0000-0003-1704-597X
Moresi, Louis0000-0003-3685-174X
Additional Information:© 1998 by the American Geophysical Union. Received August 4, 1997; revised February 1, 1998; accepted February 12, 1998. This work is supported by the David and Lucile Packard Foundation and NSF grant EAR-9417645. We thank Hiroo Kanamori for many enlightening discussions and David Bercovici and Paul Tackley for reviewing the paper. Some of the calculations were carried out on the Intel Paragon supercomputer at Caltech's Center for Advanced Computer Research. This is contribution 6204 of the Division of Geological and Planetary Sciences, California Institute of Technology.
Group:Seismological Laboratory
Funders:
Funding AgencyGrant Number
David and Lucile Packard FoundationUNSPECIFIED
NSFEAR-9417645
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Caltech Division of Geological and Planetary Sciences6204
Record Number:CaltechAUTHORS:20130123-074905905
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20130123-074905905
Official Citation:Zhong, S., M. Gurnis, and L. Moresi (1998), Role of faults, nonlinear rheology, and viscosity structure in generating plates from instantaneous mantle flow models, J. Geophys. Res., 103(B7), 15255–15268, doi:10.1029/98JB00605
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:36520
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:24 Jan 2013 19:39
Last Modified:24 Oct 2017 18:38

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