Dynamics of Plate Tectonics and Mantle Flow: From Local to Global Scales
Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global mantle flow remain a computational challenge. We capitalized on advances in adaptive mesh refinement algorithms on parallel computers to sim...
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| Published in | Science (American Association for the Advancement of Science) Vol. 329; no. 5995; pp. 1033 - 1038 |
|---|---|
| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Washington, DC
American Association for the Advancement of Science
27.08.2010
The American Association for the Advancement of Science |
| Subjects | |
| Online Access | Get full text |
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| Abstract | Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global mantle flow remain a computational challenge. We capitalized on advances in adaptive mesh refinement algorithms on parallel computers to simulate global mantle flow by incorporating plate motions, with individual plate margins resolved down to a scale of 1 kilometer. Back-arc extension and slab rollback are emergent consequences of slab descent in the upper mantle. Cold thermal anomalies within the lower mantle couple into oceanic plates through narrow high-viscosity slabs, altering the velocity of oceanic plates. Viscous dissipation within the bending lithosphere at trenches amounts to approximately 5 to 20% of the total dissipation through the entire lithosphere and mantle. |
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| AbstractList | Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global mantle now remain a computational challenge. We capitalized on advances in adaptive mesh refinement algorithms on parallel computers to simulate global mantle now by incorporating plate motions, with individual plate margins resolved down to a scale of 1 kilometer. Back-arc extension and slab rollback are emergent consequences of slab descent in the upper mantle. Cold thermal anomalies within the lower mantle couple into oceanic plates through narrow high-viscosity slabs, altering the velocity of oceanic plates. Viscous dissipation within the bending lithosphère at trenches amounts to ~5 to 20% of the total dissipation through the entire lithosphère and mantle. Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global mantle flow remain a computational challenge. We capitalized on advances in adaptive mesh refinement algorithms on parallel computers to simulate global mantle flow by incorporating plate motions, with individual plate margins resolved down to a scale of 1 kilometer. Back-arc extension and slab rollback are emergent consequences of slab descent in the upper mantle. Cold thermal anomalies within the lower mantle couple into oceanic plates through narrow high-viscosity slabs, altering the velocity of oceanic plates. Viscous dissipation within the bending lithosphere at trenches amounts to approximately 5 to 20% of the total dissipation through the entire lithosphere and mantle. Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global mantle flow remain a computational challenge. We capitalized on advances in adaptive mesh refinement algorithms on parallel computers to simulate global mantle flow by incorporating plate motions, with individual plate margins resolved down to a scale of 1 kilometer. Back-arc extension and slab rollback are emergent consequences of slab descent in the upper mantle. Cold thermal anomalies within the lower mantle couple into oceanic plates through narrow high-viscosity slabs, altering the velocity of oceanic plates. Viscous dissipation within the bending lithosphere at trenches amounts to ~5 to 20% of the total dissipation through the entire lithosphere and mantle. [PUBLICATION ABSTRACT] Improving Earth Models The geophysical processes responsible for shaping the planet's surface and interior need largescale simulations, but to achieve high resolution at these scales is costly and tends to focus on gradual processes such as plate tectonics. By using large parallel supercomputers, Stadler et al. (p. 1033 ; see the Perspective by Becker ; see the cover) have improved on a commonly used method—adaptive mesh refinement—to increase the resolution of global geodynamic models to the scale of a single kilometer and been able to reveal unexpected insights into localized processes, such as subduction zone mechanics, thermal anomalies in the lower mantle, and the speed of movement of oceanic plates. Computational advances enable the modeling of global geophysical processes to the scale of a kilometer. Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global mantle flow remain a computational challenge. We capitalized on advances in adaptive mesh refinement algorithms on parallel computers to simulate global mantle flow by incorporating plate motions, with individual plate margins resolved down to a scale of 1 kilometer. Back-arc extension and slab rollback are emergent consequences of slab descent in the upper mantle. Cold thermal anomalies within the lower mantle couple into oceanic plates through narrow high-viscosity slabs, altering the velocity of oceanic plates. Viscous dissipation within the bending lithosphere at trenches amounts to ~5 to 20% of the total dissipation through the entire lithosphere and mantle. |
| Author | Wilcox, Lucas C Ghattas, Omar Burstedde, Carsten Alisic, Laura Gurnis, Michael Stadler, Georg |
| Author_xml | – sequence: 1 fullname: Stadler, Georg – sequence: 2 fullname: Gurnis, Michael – sequence: 3 fullname: Burstedde, Carsten – sequence: 4 fullname: Wilcox, Lucas C – sequence: 5 fullname: Alisic, Laura – sequence: 6 fullname: Ghattas, Omar |
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| Keywords | plate movement strain rates algorithms models simulation thermal anomalies lithosphere velocity plate tectonics dynamics viscosity extension tectonics back-arc basins mantle subduction zones plate boundaries flow trenches oceanic crust high resolution |
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| Snippet | Plate tectonics is regulated by driving and resisting forces concentrated at plate boundaries, but observationally constrained high-resolution models of global... Improving Earth Models The geophysical processes responsible for shaping the planet's surface and interior need largescale simulations, but to achieve high... |
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| SubjectTerms | Algorithms Boundaries Computer simulation Convergent boundaries Dissipation Earth sciences Earth, ocean, space Earthquakes Exact sciences and technology Flow velocity Geomorphology Geophysics Internal geophysics Kinematics Kinetics Lithosphere Lower mantle Mantle Mathematical models Plate tectonics Slabs Solid-earth geophysics, tectonophysics, gravimetry Strain rate Tectonic plate interactions Tectonics. Structural geology. Plate tectonics Viscosity |
| Title | Dynamics of Plate Tectonics and Mantle Flow: From Local to Global Scales |
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