Whole-mantle convection with tectonic plates preserves long-term global patterns of upper mantle geochemistry [PDF]
Scientific Reports, 2017 The evolution of the planetary interior during plate tectonics is controlled by slow convection within the mantle. Global-scale geochemical differences across the upper mantle are known, but how they are preserved during convection has not been ...
T. L. Barry +7 more
doaj +2 more sources
Philosophical Transactions Series A, Mathematical, Physical, and Engineering Sciences, 2002 We review the present state of our understanding of mantle convection with respect to geochemical and geophysical evidence and we suggest a model for mantle convection and its evolution over the Earth's history that can reconcile this evidence. Whole-mantle convection, even with material segregated within the D" region just above the core-mantle ...
Francis Albarede, Rob D Van Der Hilst
exaly +5 more sources
On the effect of continents on mantle convection [PDF]
Journal of Geophysical Research: Solid Earth, 1995 At the Earth's surface, continents and oceans impose different thermal boundary conditions at the top of the mantle. Laboratory experiments are used to investigate the consequences of this for mantle convection. The upper boundary of the experimental tank was made of copper plates enforcing a fixed temperature and had a conductive lid of finite width ...
Guillou-Frottier, Laurent +1 more
openaire +4 more sources
On the Scales of Dynamic Topography in Whole‐Mantle Convection Models
Geochemistry, Geophysics, Geosystems, 2018 Mantle convection shapes Earth's surface by generating dynamic topography. Observational constraints and regional convection models suggest that surface topography could be sensitive to mantle flow for wavelengths as short as 1,000 and 250 km ...
Maelis Arnould +2 more
exaly +2 more sources
Continuous reorientation of synchronous terrestrial planets dueto mantle convection [PDF]
Nat Geosci, 2018 Jérémy Leconte
openalex +2 more sources
Geophysical Monograph Series, Page 137-165., 2020 This book is Open Access. A digital copy can be downloaded for free from Wiley Online Library.
Explores the behavior of carbon in minerals, melts, and fluids under extreme conditions
Carbon trapped in diamonds and carbonate-bearing rocks in subduction zones are examples of the continuing exchange of substantial carbon ...
Konstantin Litasov +3 more
wiley +6 more sources
Geophysical Monograph Series, Page 435-447., 2021 Exploring the links between Large Igneous Provinces and dramatic environmental impact
An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Peter E. Marshall +2 more
wiley +4 more sources
Timescales of chemical equilibrium between the convecting solid mantle and over- and underlying magma oceans [PDF]
Solid Earth, 2021 After accretion and formation, terrestrial planets go through at least one magma ocean episode. As the magma ocean crystallises, it creates the first layer of solid rocky mantle.
D. P. Bolrão +7 more
doaj +1 more source
Effects of Composite Rheology on Plate‐Like Behavior in Global‐Scale Mantle Convection
Geophysical Research Letters, 2023 Earth's upper mantle rheology controls lithosphere‐asthenosphere coupling and thus surface tectonics. Rock deformation experiments and seismic anisotropy measurements indicate that composite rheology (co‐existing diffusion and dislocation creep) occurs ...
Maëlis Arnould +2 more
doaj +1 more source
Narrow, Fast, and “Cool” Mantle Plumes Caused by Strain‐Weakening Rheology in Earth's Lower Mantle
Geochemistry, Geophysics, Geosystems, 2022 The rheological properties of Earth's lower mantle are key for mantle dynamics and planetary evolution. The main rock‐forming minerals in the lower mantle are bridgmanite (Br) and smaller amounts of ferropericlase (Fp).
A. J. P. Gülcher +4 more
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