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On the Relative Importance of the Driving Forces of Plate Motion
Open accessAbstract
A number of possible mechanisms have recently been proposed for driving the motions of the lithospheric plates, such as pushing from mid-ocean ridges, pulling by downgoing slabs, suction toward trenches, and coupling of the plates to flow in the mantle. We advance a new observational method of testing these theories of the driving mechanism. Our basic approach is to solve the inverse problem of determining the relative strength of the plausible driving forces, given the observed motions and geometries of the lithospheric plates. Since the inertia of the plates is negligible, each plate must be in dynamic equilibrium, so that the sum of the torques acting on a plate must be zero. Thus, our problem is to determine the relative sizes of the forces that minimize the components of net torque on each plate. The results indicate that the forces acting on the downgoing slab control the velocity of the oceanic plates and are an order of magnitude stronger than any other force. Namely, all the oceanic plates attached to substantial amounts of downgoing slabs move with a ‘terminal velocity’ at which the gravitational body force pulling the slabs downward is nearly balanced with the resistance acting on the slab; regardless of the other features of the trailing horizontal part of the plates. The drag on the bottom of the plates which resist motion is stronger under the continents than under the oceans.
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“with the gravitational pull of subducting slabs now understood to be the dominant driving force for surface plate motion”
From Secular change and the onset of plate tectonics on Earth (2020) · cites this paper as Forsyth and Uyeda, 1975
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Capitanio, F. A., Stegman, D. R., Moresi, L. N., & Sharples, W. (2009) · Tectonophysics · doi:10.1016/j.tecto.2009.08.020 · Cited by 159
Wan, B., Wu, F., Chen, L., Zhao, L., Liang, X., Xiao, W., & Zhu, R. (2019) · Science China Earth Sciences · doi:10.1007/s11430-019-9393-4 · Cited by 157
Northeast Atlantic passive continental margins: Rifting and subsidence processes
Montadert, L., de Charpal, O., Roberts, D., Guennoc, P., & Sibuet, J. (1979) · Maurice Ewing series · doi:10.1029/me003p0154 · Cited by 157
Subduction dynamics as revealed by trench migration
Lallemand, S., Heuret, A., Faccenna, C., & Funiciello, F. (2008) · Tectonics · doi:10.1029/2007tc002212 · Cited by 155
“[26] 1. The slab pull force Fsp represents the main driving force in the system [e.g., Forsyth and Uyeda, 1975; McKenzie, 1977; Davies, 1980; Carlson, 1995].”
BackgroundInfluentialFragmentation of the Farallon Plate by Pivoting Subduction
Menard, H. W. (1978) · The Journal of Geology · doi:10.1086/649658 · Cited by 156
Whole-mantle convection and plate tectonics
Davies, G. F. (1977) · Geophysical Journal International · doi:10.1111/j.1365-246x.1977.tb03717.x · Cited by 156
Heat flow, arc volcanism, and subduction in northern Oregon
Blackwell, D., Bowen, R. G., Hull, D. A., Riccio, J., & Steele, J. (1982) · Journal of Geophysical Research Atmospheres · doi:10.1029/jb087ib10p08735 · Cited by 155
Slab detachment in continental collision zones: An analysis of controlling parameters
Ton, S. Y. M. W. A., & Wortel, M. J. R. (1997) · Geophysical Research Letters · doi:10.1029/97gl01939 · Cited by 153
Double seismic zones and stresses of intermediate depth earthquakes
Fujita, K., & Kanamori, H. (1981) · Geophysical Journal International · doi:10.1111/j.1365-246x.1981.tb05950.x · Cited by 154
Oceanic lithosphere and asthenosphere: Thermal and mechanical structure
Schubert, G., Froidevaux, C., & Yuen, D. A. (1976) · Journal of Geophysical Research Atmospheres · doi:10.1029/jb081i020p03525 · Cited by 151
Intraplate Stresses: A New Element in Basin Analysis
Cloetingh, S. A. P. L. (1988) · Frontiers in sedimentary geology · doi:10.1007/978-1-4612-3788-4_10 · Cited by 152
Scotese, C. R. (2009) · Geological Society London Special Publications · doi:10.1144/sp326.4 · Cited by 150
Coltice, N., Husson, L., Faccenna, C., & Arnould, M. (2019) · Science Advances · doi:10.1126/sciadv.aax4295 · Cited by 151
“The velocity is dependent on the overall buoyancy of the slab, supporting the importance of the length of trenches rather than the depth of the slab (which does not vary as extensively as trench length), as proposed by (3).”
BackgroundGlobal upper‐mantle structure from finite‐frequency surface‐wave tomography
Zhou, Y., Nolet, G., Dahlen, F. A., & Laske, G. (2006) · Journal of Geophysical Research Atmospheres · doi:10.1029/2005jb003677 · Cited by 150
Dynamics of slab rollback and induced back-arc basin formation
Nakakuki, T., & Mura, E. (2012) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2012.10.031 · Cited by 156
An extreme-scale implicit solver for complex PDEs
Rudi, J., Malossi, A. C. I., Isaac, T., Stadler, G., Gurnis, M., Staar, P., Ineichen, Y., Bekas, C., Curioni, A., & Ghattas, O. N. (2015) · International Conference for High Performance Computing, Networking, Storage and Analysis (SC) · doi:10.1145/2807591.2807675 · Cited by 150
“The second question concerns the forces driving and resisting global plate motion and the degree to which interplate coupling governs plate motions [4], [33], [34].”
BackgroundNiu, Y. (2014) · Global Tectonics and Metallogeny · doi:10.1127/gtm/2014/0009 · Cited by 151
Metadata
- Authors
- Forsyth, D., & Uyeda, S.
- Affiliations
- Massachusetts Institute of Technology (US)
- Lamont-Doherty Earth Observatory (US)
- ORCID
- Forsyth, D.
- Venue
- Geophysical Journal International
- Publisher
- Oxford University Press (OUP)
- Published
- 1975-10-01
- Volume
- 43
- Issue
- 1
- Pages
- 163-200
- ISSN
- 0956-540X (ISSN-L)
- 1365-246X
- OpenAlex
- W2011893217
- Cited by
- 1,673
- References
- 86
- Citations by year
- 2026: 33 · 2025: 42 · 2024: 57 · 2023: 78 · 2022: 64 · 2021: 66 · 2020: 82 · 2019: 52 · 2018: 73 · 2017: 60 · 2016: 46 · 2015: 50 · 2014: 33 · 2013: 37 · 2012: 37
- FWCI
- 23.95
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Geophysical Journal International (publishedVersion)
- Funders
- National Science Foundation
- Office of Naval Research (N00014)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geophysics › earthquake and tectonic studies
- Physical Sciences › Earth and Planetary Sciences › Geology › Geological and Geophysical Studies
- Physical Sciences › Earth and Planetary Sciences › Geophysics › High-pressure geophysics and materials
- Keywords
- plate motion, plate driving forces, slab pull, inverse problems, plate tectonics
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