Results 1 to 10 of about 27,280 (282)
Convective Self‐Compression of Cratons and the Stabilization of Old Lithosphere
Despite being exposed to convective stresses for much of the Earth's history, cratonic roots appear capable of resisting mantle shearing. This tectonic stability can be attributed to the neutral density and higher strength of cratons. However, the excess
Jyotirmoy Paul +3 more
doaj +1 more source
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]
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
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
Multidisciplinary Constraints on the Thermal‐Chemical Boundary Between Earth's Core and Mantle
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
Three‐dimensional flow in the subslab mantle
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
Joint Interpretation Results of Gravitational and Thermal Fields for the Ural Region
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
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
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
Observations of seismic anisotropy just above the core‐mantle boundary are a powerful way to understand the dynamics of the lowermost mantle. Here we present models of seismic anisotropy in the lowermost mantle beneath Siberia based on new and previously
Neala Creasy +3 more
doaj +1 more source

