0000000000659718

AUTHOR

Louis Moresi

showing 3 related works from this author

The role of slabs and oceanic plate geometry in the net rotation of the lithosphere, trench motions, and slab return flow

2012

[1] Absolute plate motion models with respect to a deep mantle reference frame (e.g., hot spots) typically contain some net rotation (NR) of the lithosphere. Global mantle flow models for the present-day plate setting reproduce similarly oriented NRs but with amplitudes significantly smaller than those found in some high NR Pacific hot spot reference frames. It is therefore important to understand the mechanisms of NR excitation, which we attempt here with two-dimensional cylindrical models of an idealized Pacific domain. We study the influence of slab properties, oceanic ridge position, continental keels, and a weak asthenospheric layer on NR and trench migration. Fast slab return flow dev…

Slab suctiongeographygeography.geographical_feature_category010504 meteorology & atmospheric sciencesMid-ocean ridgeGeophysics010502 geochemistry & geophysics01 natural sciencesMantle (geology)Geophysics13. Climate actionGeochemistry and PetrologyLithosphereOceanic crustTrenchSlab windowSlabSeismologyGeology0105 earth and related environmental sciencesGeochemistry, Geophysics, Geosystems
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The Impact of a Very Weak and Thin Upper Asthenosphere on Subduction Motions

2019

Recent geophysical observations report the presence of a very weak and thin upper asthenosphere underneath subducting oceanic plates at convergent margins. Along these margins, trench migrations are significantly slower than plate convergence rates. We use numerical models to assess the role of a weak upper asthenospheric layer on plate and trench motions. We show that the presence of this layer alone can enhance an advancing trend for the motion of the plate and hamper trench retreat. This mechanism provides a novel and alternative explanation for the slow rates of trench migration and fast-moving plates observed globally at natural subduction zones.

010504 meteorology & atmospheric sciencesSubductionNumerical models010502 geochemistry & geophysics01 natural sciencesGeophysicsMantle convectionAsthenosphereOceanic crustLithosphereTransition zoneTrenchGeneral Earth and Planetary SciencesPetrologyGeology0105 earth and related environmental sciencesGeophysical Research Letters
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The role of slabs and oceanic plate geometry in the net rotation of the lithosphere, trench motions, and slab return flow

2012

International audience; [1] Absolute plate motion models with respect to a deep mantle reference frame (e.g., hot spots) typically contain some net rotation (NR) of the lithosphere. Global mantle flow models for the present-day plate setting reproduce similarly oriented NRs but with amplitudes significantly smaller than those found in some high NR Pacific hot spot reference frames. It is therefore important to understand the mechanisms of NR excitation, which we attempt here with two-dimensional cylindrical models of an idealized Pacific domain. We study the influence of slab properties, oceanic ridge position, continental keels, and a weak asthenospheric layer on NR and trench migration. F…

[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicstrench motions.slab dynamics[SDE.MCG]Environmental Sciences/Global Changestrench motionslithosphere-mantle interactionsnet rotation of the lithosphere
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