Results 11 to 20 of about 19,207 (163)

Mantle Flow Drives the Subsidence of Oceanic Plates [PDF]

open access: yesScience, 2010
Sinking Sea Floors The depths of ocean bottoms are constantly fluctuating at a very slow rate in response to the generation (at mid-ocean ridges) and consumption (at subduction zones) of sea-floor material. Because older sea floor is susceptible to sinking as it cools, it has been assumed that sea-floor depth varies directly with
Adam, Claudia, Vidal, Valérie
openaire   +3 more sources

Martian Mantle Heat Flow Estimate From the Lack of Lithospheric Flexure in the South Pole of Mars: Implications for Planetary Evolution and Basal Melting

open access: yesGeophysical Research Letters, 2021
Heat flow measurements are important for our understanding of planetary interior composition, structure, and evolution. In the absence of direct measurement, a first‐order estimate of a planet's interior heat flow can be made by modeling the lithosphere ...
Lujendra Ojha   +6 more
doaj   +1 more source

The deep Earth origin of the Iceland plume and its effects on regional surface uplift and subsidence [PDF]

open access: yesSolid Earth, 2017
The present-day seismic structure of the mantle under the North Atlantic Ocean indicates that the Iceland hotspot represents the surface expression of a deep mantle plume, which is thought to have erupted in the North Atlantic domain during the ...
N. Barnett-Moore   +3 more
doaj   +1 more source

Mantle Flow Pattern Associated With the Patagonian Slab Window Determined From Azimuthal Anisotropy

open access: yesGeophysical Research Letters, 2022
Geological processes in Southern Patagonia are affected by the Patagonian slab window, formed by the subduction of the Chile Ridge and subsequent northward migration of the Chile Triple Junction.
Walid Ben‐Mansour   +6 more
doaj   +1 more source

A Bayesian approach to the tomographic problem with constraints from geodynamic modeling: Application to a synthetic subduction zone

open access: yesSeismica, 2022
Geodynamic tomography, an imaging technique that incorporates constraints from geodynamics and mineral physics to restrict the potential number of candidate seismic models down to a subset consistent with geodynamic predictions, is applied to a thermal ...
John Keith Magali, Thomas Bodin
doaj   +1 more source

Three‐dimensional flow in the subslab mantle

open access: yesGeochemistry, Geophysics, Geosystems, 2014
Three‐dimensional models of mantle flow at subduction zones make it possible to explain the common occurrence of trench‐parallel subslab seismic anisotropy.
Karen Paczkowski   +3 more
doaj   +1 more source

Multidisciplinary Constraints on the Thermal‐Chemical Boundary Between Earth's Core and Mantle

open access: yesGeochemistry, Geophysics, Geosystems, 2022
Heat flux from the core to the mantle provides driving energy for mantle convection thus powering plate tectonics, and contributes a significant fraction of the geothermal heat budget.
Daniel A. Frost   +9 more
doaj   +1 more source

Joint Interpretation Results of Gravitational and Thermal Fields for the Ural Region

open access: yesRussian Journal of Earth Sciences, 2023
A method for solving conjugation problems for the Poisson equation is implemented, which makes it possible to interpret potential fields (gravitational and stationary thermal fields) based on unified grid algorithms.
Martyshko Pyotr   +2 more
doaj   +1 more source

Seismic evidence for subduction-induced mantle flows underneath Middle America

open access: yesNature Communications, 2020
The motions of subducted slabs are expected to drive mantle flow around slab edges, however, evidence of deep mantle flow has so far remained elusive.
Hejun Zhu, Robert J. Stern, Jidong Yang
doaj   +1 more source

Upper Mantle Anisotropy and Flow Beneath the Pacific Ocean Revealed by Differential PS‐SKS Splitting

open access: yesGeophysical Research Letters, 2023
Upper mantle anisotropy has been mapped beneath continents at high spatial resolution. Beneath the oceans, however, shear wave splitting constraints on upper mantle anisotropy are sparse, due to the paucity of seismic receivers. A technique that does not
Jonathan Wolf, Maureen D. Long
doaj   +1 more source

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