The Quest for self-consistent generation of plate tectonics in mantle convection models

scientific article published in 2000

The Quest for self-consistent generation of plate tectonics in mantle convection models is …
instance of (P31):
scholarly articleQ13442814

External links are
P356DOI10.1029/GM121P0047

P50authorPaul J TackleyQ59811215
P2860cites workMantle convection with a brittle lithosphere: thoughts on the global tectonic styles of the Earth and VenusQ29394773
Global tectonics and space geodesyQ33295767
A three-dimensional self-consistent computer simulation of a geomagnetic field reversalQ55879456
Neoproterozoic-Paleozoic geography and tectonics: Review, hypothesis, environmental speculationQ55880623
A sensitivity study of three-dimensional spherical mantle convection at 108Rayleigh number: Effects of depth-dependent viscosity, heating mode, and an endothermic phase changeQ55970161
Seismological evidence for a lithospheric normal faulting — the Sanriku earthquake of 1933Q56067358
Composition and development of the continental tectosphereQ56136740
Structure and Formation of the Continental TectosphereQ56136780
Cratonization and thermal evolution of the mantleQ56656991
Large-scale mantle convection and the aggregation and dispersal of supercontinentsQ56772344
CRUST 5.1: A global crustal model at 5° × 5°Q57308373
Mantle dynamics and the heat flow into the Earth's continentsQ59039821
Mantle convection simulations with rheologies that generate plate-like behaviourQ59069900
An Earth-like numerical dynamo modelQ59091124
The continental tectosphereQ59407163
Some thoughts on the stability of cratonic lithosphere: Effects of buoyancy and viscosityQ59712970
Shear deformation zones along major transform faults and subducting slabsQ59748722
Toroidal-poloidal partitioning of plate motions since 120 MAQ59798613
Interaction of weak faults and non-newtonian rheology produces plate tectonics in a 3D model of mantle flowQ60084260
A source-sink model of the generation of plate tectonics from non-Newtonian mantle flowQ60714236
On the purpose of toroidal motion in a convecting mantleQ60714237
A continuous kinematic model of plate-tectonic motionsQ60714238
A simple model of plate generation from mantle flowQ60714242
On the equipartition of kinetic energy in plate tectonicsQ60714247
Rapid drift of large continents during the late Precambrian and Paleozoic: Paleomagnetic constraints and dynamic modelsQ61662487
Mantle convection with plates and mobile, faulted plate marginsQ81125369
Water in the oceanic upper mantle: implications for rheology, melt extraction and the evolution of the lithosphereQ97322608
Crustal thickening versus lateral expulsion in the Indian-Asian continental collisionQ97449351
Extension of stable continental lithosphere and the initiation of lithospheric scale faultsQ97485574
Strength of the lithosphere: Constraints imposed by laboratory experimentsQ98962720
Jurassic and cretaceous plate tectonic reconstructionsQ99916216
A simple parameterization of strain localization in the ductile regime due to grain size reduction: A case study for olivineQ105127358
Mantle convection model with a dynamic plate: topography, heat flow and gravity anomaliesQ107112729
Punctuated tectonic evolution of the earthQ107275038
Thermal and mechanical evolution of shear zonesQ107407686
P921main subjectplate tectonicsQ7950
P304page(s)47-72
P577publication date2000-01-01
P1433published inGeophysical MonographQ29043683
P1476titleThe Quest for self-consistent generation of plate tectonics in mantle convection models

Reverse relations

cites work (P2860)
Q60714195A continuum theory of grain size evolution and damage
Q92081282Diffuse oceanic plate boundaries: Strain rates, vertically averaged rheology, and comparisons with narrow plate boundaries and stable plate interiors
Q107297128Generation of plate-like behavior and mantle heterogeneity from a spherical, viscoplastic convection model
Q60714212Tectonic plate generation and two-phase damage: Void growth versus grain size reduction
Q60714216The generation of plate tectonics from mantle convection

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