Results 51 to 60 of about 4,195 (236)

On the evolution of the water ocean in the plate-mantle system

open access: yesProgress in Earth and Planetary Science, 2018
Here, we investigate a possible scenario of surface seawater evolution in the numerical simulations of surface plate motion driven by mantle dynamics, including thermo-chemical convection and water migration, from the early to present-day Earth to ...
Takashi Nakagawa   +3 more
doaj   +1 more source

Tectonic plates in 3D mantle convection model with stress-history-dependent rheology

open access: yesEarth, Planets and Space, 2020
Plate tectonics is a key feature of the dynamics of the Earth’s mantle. By taking into account the stress-history-dependent rheology of mantle materials, we succeeded in realistically producing tectonic plates in our numerical model of mantle convection ...
Takehiro Miyagoshi   +2 more
doaj   +1 more source

How Phase Transitions Impact Changes in Mantle Convection Style Throughout Earth's History: From Stalled Plumes to Surface Dynamics

open access: yesGeochemistry, Geophysics, Geosystems
Mineral phase transitions can either hinder or accelerate mantle flow. In the present day, the formation of the bridgmanite + ferropericlase assemblage from ringwoodite at 660 km depth has been found to cause weak and intermittent layering of mantle ...
Ranpeng Li   +4 more
doaj   +1 more source

Intraplate Seamounts as a Window into Deep Earth Processes [PDF]

open access: yesOceanography, 2010
Seamounts are windows into the deep Earth that are helping to elucidate various deep Earth processes. For example, thermal and mechanical properties of oceanic lithosphere can be deter-mined from the flexing of oceanic crust caused by the growth of ...
Anthony A.P. Koppers, Anthony B. Watts
doaj  

A Simple Thermodynamic Model of the Internal Convective Zone of the Earth

open access: yesEntropy, 2018
As it is well known both atmospheric and mantle convection are very complex phenomena. The dynamical description of these processes is a very difficult task involving complicated 2-D or 3-D mathematical models.
Karen Arango-Reyes   +3 more
doaj   +1 more source

3D Variations in Viscosity Reconcile the Strength of the Lower Mantle Inferred From Glacial Isostatic Adjustment and Mantle Convection

open access: yesGeophysical Research Letters
A widely accepted global model of glacial isostatic adjustment (GIA) is based on ICE‐6G ice loading and 1D‐viscosity model VM5a, a viscosity profile which remains at odds with mantle convection constraints such as from geoid modeling.
A. Bellas‐Manley   +3 more
doaj   +1 more source

On the impact of true polar wander on heat flux patterns at the core–mantle boundary [PDF]

open access: yesSolid Earth
The heat flux across the core–mantle boundary (CMB) is a fundamental variable for Earth evolution and internal dynamics. Seismic tomography provides access to seismic heterogeneities in the lower mantle, which can be related to present-day thermal ...
T. Frasson   +4 more
doaj   +1 more source

MANTLE CONVECTION FOR GEOLOGISTS [PDF]

open access: yesAmerican Mineralogist, 2014
By Geoffrey F. Davies (2011) Cambridge University Press, U.K., 232 p. $64.00 ISBN 978-0-521-19800-4 (Hardback; e-formats available). Since the plate tectonics model was advanced in the 1960s, mantle convection has been recognized to be at the heart of various activities of the solid Earth like volcanism, continental drift, mountain building, and ...
openaire   +1 more source

Effects of adiabatic compression on thermal convection in super-Earths of various sizes

open access: yesEarth, Planets and Space, 2018
We present two-dimensional numerical models of thermal convection of a compressible fluid in the mantles of super-Earths calculated under the truncated anelastic liquid approximation to discuss how adiabatic compression affects the thermal convection ...
Takehiro Miyagoshi   +2 more
doaj   +1 more source

Lithosphere‐Asthenosphere Interactions Across the Indo‐Burma Subduction Zone From Sp Receiver Functions

open access: yesGeophysical Research Letters, Volume 53, Issue 11, 16 June 2026.
Abstract The Cenozoic convergence between the Indian and Asian plates has driven large‐scale mantle convection that interacts with both plates. Understanding this convergence benefits from clear imaging of the lithosphere‐asthenosphere boundary (LAB).
Yiming Bai   +12 more
wiley   +1 more source

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