Dynamics of Subducting Slabs: Numerical Modeling and Constraints from Seismology, Geoid, Topography, Geochemistry, and Petrology

No abstract is available for this paper.

• Publication year

  2015

• Venue

  Unknown venue

• Publication date

  Unknown publication date

• Fields of study

  Physics, Environmental Science, Geology

• Identifiers
  DOI 10.1016/B978-0-444-53802-4.00132-9
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

• Thermal and petrologic structure of subduction zones

  2013cited by this paper
• On the Competing Roles of Fault Reactivation and Brittle Failure in Generating Plate Tectonics from Mantle Convection

  2013cited by this paper
• What Controls the Seismogenic Plate Interface in Subduction Zones

  2013cited by this paper
• Mantle flow in subduction systems: The mantle wedge flow field and implications for wedge processes

  2013cited by this paper
• Generation of plate tectonics with two-phase grain-damage and pinning: Source–sink model and toroidal flow

  2013cited by this paper
• The influence of mantle internal heating on lithospheric mobility: Implications for super-Earths

  2013cited by this paper
• Experimental constraints on melt generation in the mantle wedge

  2013cited by this paper
• Thermal Structure and Metamorphic Evolution of Subducting Slabs

  2013cited by this paper
• CONSTRAINTS ON SUBDUCTION GEODYNAMICS FROM SEISMIC ANISOTROPY

  2013cited by this paper
• The Transition‐Zone Water Filter Model for Global Material Circulation: Where Do We Stand?

  2013cited by this paper
• Geochemical Fluxes During Seafloor Alteration of the Basaltic Upper Oceanic Crust: DSDP Sites 417 and 418

  2013cited by this paper
• The Relation Between Mantle Dynamics and Plate Tectonics: A Primer

  2013cited by this paper
• Tracers of the Slab

  2013cited by this paper
• Aspherical Structure of the Mantle, Tectonic Plate Motions, Nonhydrostatic Geoid, and Topography of the Core‐Mantle Boundary

  2013cited by this paper
• Boron and Other Fluid‐mobile Elements in Volcanic Arc Lavas: Implications for Subduction Processes

  2013cited by this paper
• Thermal Structure due to Solid‐State Flow in the Mantle Wedge Beneath Arcs

  2013cited by this paper
• Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs

  2012cited by this paper
• Effects of heterogeneous hydration in the incoming plate, slab rehydration, and mantle wedge hydration on slab-derived H 2 O flux in subduction zones

  2012cited by this paper
• The conditions for plate tectonics on super-Earths: Inferences from convection models with damage

  2012cited by this paper
• Juan de Fuca slab geometry and its relation to Wadati-Benioff zone seismicity

  2012cited by this paper
• P wave anisotropic tomography of the Nankai subduction zone in Southwest Japan

  2012cited by this paper
• Anisotropic uppermost mantle in young subducted slab underplating Central Mexico

  2012cited by this paper
• Nazca–South America interactions and the late Eocene–late Oligocene flat‐slab episode in the central Andes

  2012cited by this paper
• Archean Subduction: Fact or Fiction?

  2012cited by this paper
• LLNL‐G3Dv3: Global P wave tomography model for improved regional and teleseismic travel time prediction

  2012cited by this paper
• The role of rheology and slab shape on rapid mantle flow: Three‐dimensional numerical models of the Alaska slab edge

  2012cited by this paper
• Shear wave reflectivity imaging of the Nazca‐South America subduction zone: Stagnant slab in the mantle transition zone?

  2012cited by this paper
• The bending mechanics in a dynamic subduction system: Constraints from numerical modelling and global compilation analysis

  2012cited by this paper
• Sensitivity of the short- to intermediate-wavelength geoid to rheologic structure in subduction zones

  2012cited by this paper
• Co‐seismic deformation of deep slabs based on summed CMT data

  2012cited by this paper
• Three-dimensional thermal structure of subduction zones: effects of obliquity and curvature

  2012cited by this paper
• Multiple layers of seismic anisotropy and a low‐velocity region in the mantle wedge beneath Japan: Evidence from teleseismic receiver functions

  2012cited by this paper
• Fluid flow during slab unbending and dehydration: Implications for intermediate‐depth seismicity, slab weakening and deep water recycling

  2012cited by this paper
• The development and evaluation of the Earth Gravitational Model 2008 (EGM2008)

  2012cited by this paper
• How large is the subducted water flux? New constraints on mantle regassing rates

  2012cited by this paper
• A comparison of numerical surface topography calculations in geodynamic modelling: an evaluation of the ‘sticky air’ method

  2012cited by this paper
• Global variations in H2O/Ce: 1. Slab surface temperatures beneath volcanic arcs

  2012cited by this paper
• Thermal structure and intermediate-depth seismicity in the Tohoku-Hokkaido subduction zones

  2012cited by this paper
• Generation of ascending flows in the Big Mantle Wedge (BMW) beneath northeast Asia induced by retreat and stagnation of subducted slab

  2012cited by this paper
• Mantle dynamics in super-Earths: Post-perovskite rheology and self-regulation of viscosity

  2012cited by this paper
• Controls of faulting and reaction kinetics on serpentinization and double Benioff zones

  2012cited by this paper
• Electromagnetic detection of plate hydration due to bending faults at the Middle America Trench

  2012cited by this paper
• Short-term episodicity of Archaean plate tectonics

  2012cited by this paper
• Mechanisms for the generation of plate tectonics by two-phase grain-damage and pinning

  2012cited by this paper
• nfluences of the buoyancy of partially molten rock on 3-D plume patterns and elt productivity above retreating slabs

  2011cited by this paper
• Hydrogeology and Mechanics of Subduction Zone Forearcs: Fluid Flow and Pore Pressure

  2011cited by this paper
• Rheological structure of the mantle of a super-Earth: Some insights from mineral physics

  2011cited by this paper
• Subduction factory: 4. Depth-dependent flux of H2O from subducting slabs worldwide

  2011cited by this paper
• Fluidity: A fully unstructured anisotropic adaptive mesh computational modeling framework for geodynamics

  2011cited by this paper
• Plate tectonics on super-Earths: Equally or more likely than on Earth

  2011cited by this paper
• Dynamic buckling of subducting slabs reconciles geological and geophysical observations

  2011cited by this paper
• Grain-size distribution in the mantle wedge of subduction zones

  2011cited by this paper
• Anisotropic viscosity changes subduction zone thermal structure

  2011cited by this paper
• Seismic anisotropy produced by serpentine in mantle wedge

  2011cited by this paper
• Future directions in subduction modeling

  2011cited by this paper
• Flow in the Mantle Inferred from the Low Degree Harmonics of the Geopotential

  2010cited by this paper
• he global range of subduction zone thermal models

  2010cited by this paper
• The Dynamics of Plate Tectonics and Mantle Flow: From Local to Global Scales

  2010cited by this paper
• Constraints on viscous dissipation of plate bending from compressible mantle convection

  2010cited by this paper
• ON THE LIKELIHOOD OF PLATE TECTONICS ON SUPER-EARTHS: DOES SIZE MATTER?

  2010cited by this paper
• Frequency-dependent shear wave splitting beneath the Japan and Izu-Bonin subduction zones

  2010cited by this paper
• Slab stress and strain rate as constraints on global mantle flow

  2010cited by this paper
• Computational Methods for Geodynamics

  2010cited by this paper
• Dynamical consequences in the lower mantle with the post-perovskite phase change and strongly depth-dependent thermodynamic and transport properties

  2010cited by this paper
• Global slab deformation and centroid moment tensor constraints on viscosity

  2010cited by this paper
• Existence of interplane earthquakes and neutral stress boundary between the upper and lower planes of the double seismic zone beneath Tohoku and Hokkaido, northeastern Japan

  2010cited by this paper
• A community benchmark for 2-D Cartesian compressible convection in the Earth's mantle

  2010cited by this paper
• Subduction initiation at passive margins: Numerical modeling

  2010cited by this paper
• Viscosity in transition zone and lower mantle: Implications for slab penetration

  2010cited by this paper
• A simple three-dimensional model of thermo–chemical convection in the mantle wedge

  2010cited by this paper
• A regime diagram for subduction styles from 3-D numerical models of free subduction

  2010cited by this paper
• Reconciling surface plate motions with rapid three-dimensional mantle flow around a slab edge

  2010cited by this paper
• Flattening of the Earth: further from hydrostaticity than previously estimated

  2010cited by this paper
• Dynamical mechanisms controlling formation and avalanche of a stagnant slab

  2010cited by this paper
• High-pressure Hydrous Phase Relations of Radiolarian Clay and Implications for the Involvement of Subducted Sediment in Arc Magmatism

  2010cited by this paper
• Effect of mantle compressibility on the thermal and flow structures of the subduction zones

  2009cited by this paper
• Elevated fluid pressure and extreme mechanical weakness of a plate boundary thrust, Nankai Trough subduction zone

  2009cited by this paper
• Trench-parallel fast axes of seismic anisotropy due to fluid-filled cracks in subducting slabs

  2009cited by this paper
• Shear Wave Splitting and Mantle Anisotropy: Measurements, Interpretations, and New Directions

  2009cited by this paper
• Seismic evidence for thermally‐controlled dehydration reaction in subducting oceanic crust

  2009cited by this paper
• A Review of the Role of Subduction Dynamics for Regional and Global Plate Motions

  2009cited by this paper
• Thermal structure and geodynamics of subduction zones

  2009cited by this paper
• Characterizing the seismogenic zone of a major plate boundary subduction thrust: Hikurangi Margin, New Zealand

  2009cited by this paper
• Geochemical and numerical constraints on Neoarchean plate tectonics

  2009cited by this paper
• Tearing of Stagnant Slab

  2009cited by this paper
• Seismic structure beneath the Rivera subduction zone from finite‐frequency seismic tomography

  2009cited by this paper
• Emergence of a low-viscosity channel in subduction zones through the coupling of mantle flow and thermodynamics

  2009cited by this paper
• Kinematic variables and water transport control the formation and location of arc volcanoes

  2009cited by this paper
• Subducted slabs and lateral viscosity variations: effects on the long-wavelength geoid

  2009cited by this paper
• Parallel scalable adjoint-based adaptive solution of variable-viscosity Stokes flow problems

  2009cited by this paper
• Deep slab hydration induced by bending-related variations in tectonic pressure

  2009cited by this paper
• Deep mantle forces and the uplift of the Colorado Plateau

  2009cited by this paper
• Water‐induced convection in the Earth's mantle transition zone

  2009cited by this paper
• Common depth of slab‐mantle decoupling: Reconciling diversity and uniformity of subduction zones

  2009cited by this paper
• Determination of the pore fluid pressure ratio at seismogenic megathrusts in subduction zones: Implications for strength of asperities and Andean‐type mountain building

  2009cited by this paper
• Incorporating self‐consistently calculated mineral physics into thermochemical mantle convection simulations in a 3‐D spherical shell and its influence on seismic anomalies in Earth's mantle

  2009cited by this paper
• Seismic anisotropy of the Pacific slab and mantle wedge beneath the Japanese islands

  2009cited by this paper
• Pore pressure development beneath the décollement at the Nankai subduction zone: Implications for plate boundary fault strength and sediment dewatering

  2009cited by this paper
• Stagnant slab : A review

  2009cited by this paper
• Seismic image and origin of the Changbai intraplate volcano in East Asia: Role of big mantle wedge above the stagnant Pacific slab

  2009cited by this paper

• A divergence free C0-RIPG stream function formulation of the incompressible Stokes system with variable viscosity

  2023cites this paper
• An introductory review of the thermal structure of subduction zones: I—motivation and selected examples

  2023cites this paper
• Stagnant Slabs and Their Return Flows From Finite‐Frequency Tomography of the 410‐km and 660‐km Discontinuities

  2021cites this paper
• Evolution and demise of passive margins through grain mixing and damage

  2021cites this paper
• Two styles of plate tectonics in Earth's history.

  2020cites this paper
• Mantle Convection in Terrestrial Planets

  2020influential citation
• A simple toy model for coupled retreat and detachment of subducting slabs

  2019cites this paper
• Multimode 3‐D Kirchhoff Migration of Receiver Functions at Continental Scale

  2019cites this paper
• Numerical Modeling of Tectonic Processes

  2019cites this paper
• Boninite and boninite-series volcanics in northern Zambales ophiolite: doubly vergent subduction initiation along Philippine Sea plate margins

  2018cites this paper
• Subduction flux modulates the geomagnetic polarity reversal rate

  2018cites this paper
• Progress in numerical modeling of subducting plate dynamics

  2018cites this paper
• Three‐dimensional numerical modeling of thermal regime and slab dehydration beneath Kanto and Tohoku, Japan

  2017cites this paper
• Modelling the interplate domain in thermo-mechanical simulations of subduction: Critical effects of resolution and rheology, and consequences on wet mantle melting

  2017cites this paper
• A mantle convection perspective on global tectonics

  2017cites this paper
• Reconciling laboratory and observational models of mantle rheology in geodynamic modelling

  2016cites this paper
• Continental versus oceanic subduction zones

  2016cites this paper