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Structure and dynamics of the oceanic lithosphere-asthenosphere system
The thermochemical evolution of oceanic lithosphere and its interaction with the underlying
asthenosphere exerts a fundamental control on the dynamics of the Earth system. Since the …
asthenosphere exerts a fundamental control on the dynamics of the Earth system. Since the …
Oceanic residual depth measurements, the plate cooling model, and global dynamic topography
Convective circulation of the mantle causes deflections of the Earth's surface that vary as a
function of space and time. Accurate measurements of this dynamic topography are …
function of space and time. Accurate measurements of this dynamic topography are …
Reassessing the thermal structure of oceanic lithosphere with revised global inventories of basement depths and heat flow measurements
Half‐space cooling and plate models of varying complexity have been proposed to account
for changes in basement depth and heat flow as a function of lithospheric age in the oceanic …
for changes in basement depth and heat flow as a function of lithospheric age in the oceanic …
Joint flexural-density modeling of the Taltal, Copiapó, and Iquique hotspot ridges and the surrounding oceanic plate, offshore Chile
Based on gravity and bathymetric data and using a novel two-dimensional joint flexural-
density modeling approach, this work studies the physical properties of the oceanic Nazca …
density modeling approach, this work studies the physical properties of the oceanic Nazca …
Outer trench slope flexure and faulting at Pacific basin subduction zones
Flexure and fracturing of the seafloor on the outer trench wall of subduction zones reflect
bending of the lithosphere beyond its elastic limit. To investigate these inelastic processes …
bending of the lithosphere beyond its elastic limit. To investigate these inelastic processes …
Elasto-plastic deformation and plate weakening due to normal faulting in the subducting plate along the Mariana Trench
We investigated variations in the elasto-plastic deformation of the subducting plate along the
Mariana Trench through an analysis of flexural bending and normal fault characteristics …
Mariana Trench through an analysis of flexural bending and normal fault characteristics …
Active faulting in apparently stable peninsular India: Rift inversion and a Holocene‐age great earthquake on the Tapti Fault
We present observations of active faulting within peninsular India, far from the surrounding
plate boundaries. Offset alluvial fan surfaces indicate one or more magnitude 7.6–8.4 thrust …
plate boundaries. Offset alluvial fan surfaces indicate one or more magnitude 7.6–8.4 thrust …
Yield failure of the subducting plate at the Mariana Trench
Two tectonic plates converge at subduction zones where the subducting plate bends.
Flexural bending of a subducting plate at a trench results in pervasive normal faulting …
Flexural bending of a subducting plate at a trench results in pervasive normal faulting …
The role of viscoelasticity in subducting plates
Subduction of tectonic plates into Earth's mantle occurs when one plate bends beneath
another at convergent plate boundaries. The characteristic time of deformation at these …
another at convergent plate boundaries. The characteristic time of deformation at these …
Elastic properties of thermally treated diabase and peridotite: Implications toward the elastic properties of oceanic lithosphere
Supported by laboratory experimental results, the reduction in elastic thickness () and
flexural rigidity () at trench outer rise, which enables bending, is attributed to damage. A …
flexural rigidity () at trench outer rise, which enables bending, is attributed to damage. A …